Skip to main content

Full text of "Geology of the California continental margin : explanation of the California continental margin geologic map series : interpretive methods, symbology, stratigraphic units, and bibliography"

See other formats


♦  -^ 


A 


:  3> 


JLOGY  OF  THE 
CALIFORNIA  CONTINENTAL  MARGIN 

EXPLANATION  OF  THE 

CALIFORNIA  CONTINENTAL  MARGIN 

GEOLOGIC  MAP  SERIES 


fmm  SCIENCES 

UC  DAVIS    'ii 


7 


A   .••<1 


.'-  .<  ..';_ '  M.  jf*!'' 


.?>-■'■ 


•m4 


BULLETIN    207 


THE  RESOURCES  AGENCY 

GORDON  K   VAN  VLECK 
SECRETARY  FOR  RESOURCES 


STATE  OF  CALIFORNIA 

GEORGE  DEUKMEJiAN 
GOVERNOR 


DEPARTMENT  OF  CONSERVATION 

HANUALL  M    WARD 
DIRECTOR 


DIVISION  OF  MINES  AND  GEOLOGY 

BRIAN  E.  TUCKER 

ACTING  STA  TE  GEOLOGIST 


BULLETIN  207 

GEOLOGY  OF  THE 
CALIFORNIA  CONTINENTAL  MARGIN: 

EXPLANATION  OF  THE 
CALIFORNIA  CONTINENTAL  MARGIN 
GEOLOGIC  MAP  SERIES- 
INTERPRETIVE  METHODS 
SYMBOLOGY,  STRATIGRAPHIC  UNITS, 
AND  BIBLIOGRAPHY 

By 

Michael  P.  Kennedy 

H.  Gary  Greene* 

and 
Samuel  H.  Clarke 


1987 


UNIVERSITY    OF    CALIFORNIA 

MAR  1  ;i  1989 

GOVl.  UOCS.  -  LiukARY 


Prepared  in  cooperation  with 

the  U.S.  Geological  Survey 

and  the  California  Coastal  Comnnission 


The  project  was  funded  in  part  by  California  Coastal  Com- 
mission grant  CEIP-890-3720-44-1 14-21-01 1;  the  University 
of  Texas,  Austin,  grant  14-21-0001-301 15;  and  U.S.  Geologi- 
cal Survey,  grants  14-08-0001-15858,  14-08-0001-16728 
and  14-08-0001-17694. 


California  Department  of  Conservation 

Division  of  Mines  and  Geology 

1416  Ninth  Street,  Room   1341 

Sacramento,  California  95814 


PREFACE 

The  California  Continental  Margin  Geologic  Map  Series  and  this  accompanying  bulletin 
have  taken  five  years  to  complete.  This  work  could  not  have  been  done  without  the  assistance 
and  encouragement  of  many  enthusiastic  and  supportive  people.  The  idea  of  prcxiucing  such 
a  map  series  was  conceived  in  1975  during  discussions  between  the  U.S.  Geological  Survey 
(USGS)  and  the  California  Coastal  Commission  (CCC),  while  formulating  the  Geological 
Element  to  the  California  Coastal  Plan.  However,  it  was  not  until  1980  that  enough  data  were 
available  for  work  to  begin,  and  at  that  time  the  California  Department  of  Conservation's 
Division  of  Mines  and  Geology  (DMG),  with  partial  funding  from  the  California  Coastal 
Commission,  initiated  the  work.  Thus,  the  publications  represent  the  success  of  a  tripartite 
(DMG-CCC-USGS)  cooperative  effort  between  state  and  federal  government  agencies. 

Geology,  like  many  sciences,  is  continuously  evolving,  and  maps  portraying  geologic 
interpretations  are  thus  ephemeral.  This  map  series  is  no  exception.  However,  it  is  the  first 
standardized  offshore  geological  map  series  published  in  the  United  States,  and  it  does 
represent  a  foundation  for  detailed  marine  geological  mapping.  Many  data  voids  exist,  as 
shown  on  the  maps,  and  new  marine  geological  and  geophysical  data  are  being  collected  that 
will  gradually  improve  understanding  of  the  geology.  Therefore,  we  foresee  the  need  to 
modify  the  maps  in  the  future  and  we  hope  to  upgrade  the  series  with  periodic  reprinting. 
We  profHJse  that  new  map  sheets,  such  as  sedimentary  isopachs  and  seafloor  resources,  be 
added  to  the  series.  We  welcome  any  comment  about  the  maps,  and  are  receptive  to  construc- 
tive criticism.  We  hope  that  you  find  the  maps  and  the  method  of  offshore  geology  portrayal 
useful. 


iii 


CONTENTS 

Page 

PREFACE    iii 

INTRODUCTION    1 

INTERPRETIVE  METHODS  2 

Faults    2 

Seafloor  Stability  3 

Hydrocorbons  3 

EXPLANATION  OF  STRATIGRAPHIC  TERMINOLOGY  AND  MAP  SYMBOLOGY  4 

Strotigrophic  Units  4 

Geologic  Contacts  4 

Symbols    4 

COMPOSITE  STRATIGRAPHIC  SECTIONS 55 

BIBLIOGRAPHY    72 


ILLUSTRATIONS 

Master  legend  of  strotigrophic  units  5 

Master  explanation  of  map  symbols  6 

Figure  1.      Index  to  California  Continentol  Margin  Geologic  Map  Series       2 

Figure  2.      Location  map  of  profile  exomples 8 

Figure  3.      Location  mop  of  strotigrophic  sections     56 

Plate  1.      Master  legend  and  example  seismic  reflection  profile, 

(in  color)   with  symbols  and  terminology  In  Pocket 


Example  Seismic  Reflection  Profiles 
with  Symbols  and  Terminology 

1.  Geologic  contact   (buttress  unconformity)   9 

2.  Geologic  contact   (ponded  sediment)    10 

3.  Geologic  contact   (ponded  sediment)    11 

4.  Fault   (seafloor  expression)     12 

5.  Fault   (seafloor  expression)     13 

6.  Fault   (seafloor  expression)     14 

7.  Fault    (seafloor  expression)     15 

8.  Fault   (Quaternary)     16 

9.  Fault   (Tertiory)  17 

10.  Fault   (late  Tertiary  and  Quaternary)    18 

11.  Fault    (lote  Tertiary  and  Quaternary)     19 

12.  Fault    (late  Tertiary  and  Quaternary)     20 

13.  Fault    (late  Tertiory  and  Quaternary)     21 

14.  Fault   (thrust)     22 

15.  Fault  zone  23 

16.  Faulted  anticline    24 

17.  Fold   (anticline)  25 

18.  Fold   (anticline,  syncllne)     26 


Example  Seismic  Reflection  Profiles 
with  Symbols  and  Terminology    (continued) 

19.  Structuro!  highs  and  lows  27 

20.  Structural  high  28 

21.  Channel    (active)     29 

22.  Channel    (filled)     30 

23.  Channel   (filled)    31 

24.  Channel   (filled)     32 

25.  Channel    (buried)    33 

26.  Channel    (buried)     34 

27.  Levee  35 

28.  Landslide   (creep)    36 

29.  Landslide   (slump)   37 

30.  Landslide   (slump)   38 

31.  Landslide   (slump)    39 

32.  Landslide   (slump)   40 

33.  Landslide   (slump)   41 

34.  Landslide    (slump)   42 

35.  Landslide   (block  glide)     43 

36.  Landslide   (block  glide)     44 

37.  Landslide   (sediment  flow)    45 

38.  Gas   (seep)  46 

39.  Gas   (bright  spot,  subsurface)    47 

40.  Gas   (bright  spot,  subsurface)    48 

41.  Gas    (bright  spot,  subsurface)    49 

42.  Diapir    50 

43.  Diapir    51 

44.  Terrace    (constructional)    52 

45.  Terrace    (erosionol)  53 

46.  Terrace   (erosionol)  54 


Strotigrophic  Sections 


1.  Eel  River  Basin    57 

2.  Point  Arena  Basin  57 

3.  Bodega  Basin    58 

4.  Outer  Santo  Cruz  Basin  58 

5.  Northern  Monterey  Bay  Region   59 

6.  Southern  Monterey  Boy  Region    59 

7.  Offshore  Santa  Morio  Basin    60 

8.  Northern  Santo  Barbara  Channel 60 

9.  Santa  Ynez  Unit  and  Vicinity  61 

10.  Dos  Cuodros  Oilfield  and  Vicinity   61 

11.  Don  Miguel  Island  62 

12.  Santa  Roso  Island  63 

13.  Santa  Cruz  Island  64 

14.  Northeast  Coost  Santa  Cruz  Island   65 

15.  Offshore  Santo  Monica  Basin    65 

16.  Northern  Santo  Roso  -  Cortes  Ridge   66 

17.  Northern  Potton  Ridge    66 

18.  Santa  Cruz  •  Cotalina  Ridge    67 

19.  Son  Pedro  Basin   67 

20.  Newport  Beach  -  Dona  Point  Shelf   68 

21.  Santa  Cotalina  Island  68 

22.  San  Nicolas  Island    69 


Stratigraphic  Sections   (continued) 


23.  San  Clemente  Ridge  69 

24.  Southern  Gulf  of  Santa  Catalina  69 

25.  San  Clemente  Island  70 

26.  San  Nicolas  Basin  70 

27.  Doll  Bank    70 

28.  Thirtymile  Bank   71 

29.  Son  Diego  Shelf   71 

30.  Fortymile  Bank    71 

31.  Centrol  Blake  Knolls    72 

32.  Cortez  Bonk    72 

33.  Northeast  Bank  72 


BULLETIN  207 

GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN: 

EXPLANATION  OF  THE 

CALIFORNIA  CONTINENTAL  MARGIN 

GEOLOGIC  MAP  SERIES - 

INTERPRETIVE  METHODS 

SYMBOLOGY,  STRATIGRAPHIC  UNITS, 

AND  BIBLIOGRAPHY 


By 

Michael  P.  Kennedy',  H.  Gary  Greene', 

and  Samuel  H.  Clarke' 


INTRODUCTION 


This  bulletin  is  a  tool  for  explorationists,  planners  and 
developers  with  marine  geological,  geophysical  and  seis- 
mological  interests  in  the  California  continental  margin.  It 
was  developed  by  the  California  Department  of  Conserva- 
tion's Division  of  Mines  and  Geology,  the  U.S.  Geological 
Survey  and  the  California  Coastal  Commission.  We  have 
presented  data  primarily  in  planimetric  form  on  map 
sheets  (NOAA/NOS  1:250,000  scale)  that  cover  the  area 
from  Mexico  north  to  Oregon  and  from  the  California 
coastline  west  to  the  edge  of  the  continental  margin  (Fig- 
ure 1).  This  bulletin  is  a  companion  to  these  map  sheets, 
and  presents  an  explanation  of  the  symbols  used  in  illus- 
trations from  marine  seismic-reflection  profiles,  represent- 
ative composite  stratigraphic  columns  and  a 
comprehensive  bibliography  of  references  reviewed  or 
used  in  the  compilation  of  the  maps. 

One  of  the  principal  purposes  of  this  study  was  to  ac- 
quire and  compile  all  readily  available  geologic  data  for 
the  California  continental  margin  in  a  standard  format. 
Although  considerable  geologic  data  exist  for  this  area, 
heretofore  no  attempt  has  been  made  to  compile  and 
present  it  at  a  common  scale  with  standardized  symbolo- 

gy- 

Geologic  symbols  conventionally  used  onshore  have 
been  standardized  through  years  of  use.  Relatively  little 
effort,  however,  has  been  made  to  develop  a  standard 
format  for  many  geologic  conditions  that  arc  unique  to  the 
offshore.  Consequently,  marine  geologic  maps  that  have 
been  produced  for  offshore  arca.s  commonly  show  incon- 
sistencies in  symbology  that  lead  to  confusion  in  interpre- 


*  Colifornio  Department  of  ConMrvation,  Diviiioft  of  Min«i  and  Geology 
'  U.S.  Geological  Survey 


tation.  We  present  this  bulletin  in  an  effort  to  standardize 
the  symbols  needed  to  illustrate  geologic  phenomena  iden- 
tified by  remote  sensing  techniques  in  the  marine  environ- 
ment. We  hope  that  this  bulletin  will  assist  marine 
geologists  by  providing  a  reference  for  standard  symbols, 
and  general  users  by  providing  an  explanation  of  symbols 
used. 

Principal  sources  of  the  geologic  data  used  in  the  compi- 
lation of  this  map  series  are  published,  open-file,  and  pub- 
licly available  "in  progress"  studies.  The  types  of  data 
compiled  include,  where  available: 

1.  General  Geology:  Geologic  structures  (folds  and 
faults),  bedrock  outcrops  and  (where  possible)  ages 
and  formational  names  of  units,  submarine  landslides, 
oil  and  gas  seeps,  shallow  gas-charged  zones,  and 
areas  having  unusually  high  rates  of  erosion  or  sedi- 
ment accumulation. 

2.  Earthquake  epicenter  locations  superimposed  on  geo- 
logic structure. 

3.  Focal  mechanisms  for  selected  earthquakes  superim- 
posed on  geologic  structure. 

4.  Regional  Bouguer  gravity  anomalies  superimposed  on 
geology  and  magnetic  anomalies. 

5.  Regional  magnetic  anomalies  superimposed  on  geol- 
ogy and  gravity  data. 

6.  Geologic  hazards  (in  red). 

7.  Sources  of  data  used,  oil  and  gas  wells,  platforms,  and 
ship  (racklines  of  data  studied. 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


Figure  1.  Index  to  Colifornia  Confinental  Margin  Geologic  Mop 
Series.  Numbers  in  lower  left  hand  corners  of  boxes  refer  to  both  - 
/metric  base   sheet  used  in  the  compilation. 


INTERPRETIVE  METHODS 

Much  of  the  information  presented  on  the  maps  and  in 
this  bulletin  is  ba.sed  on  the  interpretation  of  subbottom 
seismic-reflection  data.  These  data  include  high-resolution 
reflection  profiles  gathered  with  echo  sounder,  sparker 
and  mechanical  pulsing  systems,  and  intermediate  to 
deep-penetration  profiles  gathered  with  160  kJ  sparker, 
airgun  and  watergun  systems.  Subsurface  features  ranging 
upward  in  vertical  dimension  from  approximately  1.0  m 
to  1.5  m  can  be  resolved  in  the  higher-resolution  records 
that  vary  in  subbottom  penetration  from  150  m  to  over 
400  m.  The  deep-penetration  records  used  to  determine 
deep  structure  can  resolve  features  larger  than  about  1 5  m 
in  vertical  dimension  and  commonly  record  geologic 
structure  at  subbottom  depths  of  more  than  one  kilometer. 

Ship  positioning  was  accomplished  by  range-range  pre- 
cision triangulation,  augmented  in  a  few  remote  locations 
by  satellite,  radar,  and  incrtial  navigation.  Location  accu- 
racy of  the  seismic  data  ranges  from  ab<iut  15  m  with 
precision  equipment  to  ab<iut  500  m  where  the  ship's  radar 
alone  was  used.  Although  location  accuracy  was  consid- 
ered in  the  map  compilation,  areas  and  data  sets  using 
different  navigation  techniques  arc  not  distinguished. 
Therefore,  the  IcKation  accuracy  of  mapped  geologic  fea- 
tures varies  through  each  map.  The  structural  notations 
(i.e.,  well  defined,  inferred,  and  questionable)  refer  to 
confidence  of  interpretation  of  geological  and  geophysical 
data  rather  than  IcKation. 


Standard  interpretive  methods  were  used  in  the  analysis 
of  seismic-refiection  data.  For  a  description  of  these  basic 
methods,  the  reader  is  referred  to  Moore  ( 1960)  and  Pay- 
ton  (1977).  Additional  criteria  used  to  interpret  faults, 
seafloor  stability  and  hydrocarbons  follow. 

Faults 

Criteria  used  here  for  interpretation  of  faults  are  based 
on  descriptions  by  Greene  and  others  (1973).  Well-de- 
fined faults:  ( 1 )  distinct  displacement  of  prominent  reflec- 
tors; (2)  an  abrupt  termination  of  prominent  reflectors,  or 
the  juxtaposition  of  intervals  of  prominent  reflectors  that 
have  contrasting  acoustic  characteristics;  or  (3)  an  abrupt 
change  in  the  dips  of  reflectors  across  a  distinct  boundary. 

Inferred  faults:  (1)  small  displacement  of  prominent 
reflectors,  in  which  the  upper  or  shallow  reflectors  may  be 
bent  rather  than  broken;  (2)  prominent  reflectors  that  are 
discontinuous,  and  contrasting  seismic  characteristics  that 
are  present  on  either  side  of  an  acoustically  obscure  dis- 
turbed zone;  or  (3)  apparent  changes  in  dip  on  either  side 
of  the  disturbed  zone. 

Questionable  faults  (mapped  where  obscure  interrup- 
tions of  seismic  reflectors  are  present  in  the  subsurface): 
(1)  a  shift  in  the  phase  of  reflectors;  (2)  bent  or  broken 
reflectors  that  can  be  correlated  with  known  faults  on 
other  lines;  (3)  termination  of  weak  reflectors;  or  (4)  any 
other  zone  of  seismic  contrast,  especially  where  the  zone 
appears  similar  to  and  is  aligned  with  faults  identified  on 
adjacent  lines.  Some  questionable  and  inferred  faults  have 
been  mapped  where  anomalous  tofwgraphic  lineaments 
appear  to  support  the  continuation  of  known  faults. 

The  orientation  of  faults  is  determined  principally  by 
correlation  from  one  seismic  line  to  another.  Faults  are 
correlated  between  adjacent  lines  mainly  on  the  basis  of 
their  association  with  similar  structural  and  seismic  fea- 
tures on  adjacent  profiles.  Where  fault  planes  dip  more 
than  about  35°,  the  vertical  exaggeration  common  to  seis- 
mic-reflection records  precludes  determining  the  dip,  even 
though  the  records  clearly  indicate  that  a  fault  is  present. 
Consequently,  faults  dipping  35°  or  more  are  shown  as 
vertical. 

Determining  the  amount  and  direction  of  movement  on 
a  fault  is  difficult.  Only  the  apparent  vertical  component 
(dip  separation)  of  offset  can  be  measured  on  the  seismic- 
reflection  profiles;  the  horizontal  comptinent  (strike-slip 
separation)  can  be  determined  only  where  piercing  points 
of  lines  representing  equivalent  geologic  features  can  be 
identified  on  opposite  sides  of  a  fault.  Faults  that  displace 
rocks  having  similar  acoustic  characteristics  arc  common- 
ly difficult  to  detect  on  scismic-rcfleclion  records. 

The  age  of  most  recent  faulting  as  inferred  from  seismic- 
reflection  records  is  commonly  determined  from  the  age 
of  the  youngest  reflector  cut  by  a  fault.  However,  such  age 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


assignments  may  be  complicated  by  several  factors  so  that 
they  may  not  always  accurately  reflect  fault  activity.  For 
example,  active  faults  in  some  tectonic  settings  do  not 
penetrate  rocks  near  the  earth's  surface  and  are  expressed 
instead  by  folding  at  shallow  depths.  Such  faults,  though 
active,  might  be  interpreted  as  geologically  old  fractures 
unless  associated  seismicity  indicates  modern  activity. 
Similarly,  faults  that  reach  the  seafloor  in  Tertiary  or 
pre-Tertiary  riKks  where  younger  deposits  are  absent 
might  not  be  identified  as  geologically  youthful  unless 
seismicity  data  indicate  otherwise.  Furthermore,  in  many 
areas  direct  physical  evidence  of  the  age  of  rocks  cut  by 
a  fault  is  lacking;  age  a.ssignments  in  such  cases  are  gener- 
ally rather  loosely  contrained  by  similarities  in  acoustic 
character  to  rocks  of  known  age  in  other  locations.  These 
factors  should  be  btime  in  mind  when  using  maps  derived 
from  seismic-reflection  data. 

Seafloor  Stability 

Criteria  used  for  the  interpretation  of  seafloor  stability 
are  those  described  by  Clarke  and  others  (1983,  1985). 
Subaqueous  landslides  mapped  are  mass  movements  of 
rigid  or  semi-consolidated  sediment  masses  along  discrete 
shear  surfaces,  accompanied  by  relatively  little  internal 
deformation  (Dott,  1963).  Landslides  are  commonly 
identifled  on  seismic-reflection  records  by  the  presence  (in 
longitudinal  sections)  of  some  or  all  of  the  following  char- 
acteristics: ( 1 )  a  headscarp  where  the  slip  surface  extends 
upward  to  and  is  expressed  in  the  seafloor;  (2)  compres- 
sional  ridges  and  folded  and  contorted  subbottom  reflec- 
tors resulting  from  small-scale  thrusting  and  folding  at  the 
toe  of  the  slide;  (3)  transverse  (tensional)  cracks  in  the 
body  of  the  slide;  (4)  evidence  of  rotation  or  limited  inter- 
nal deformation  of  the  reflectors;  and  (5)  the  presence  of 
a  slip  surface,  which  may  be  upwardly  concave  or  planar, 
represented  by  a  discrete  failure  plane  or  by  an  intensely 
deformed  zone  beneath  the  slide  mass. 

The  term  slump  is  commonly  applied  to  a  slide  that 
shows  evidence  of  rotational  movement  along  a  curved 
slip  surface,  and  the  term  block  glide  is  used  for  those 
landslides  having  a  relatively  planar,  usually  gently  dip- 
ping slide  surface.  Subaqueous  slides  may  occur  on  slopes 
of  less  than  one  degree  and  may  range  in  size  from  simple 
failures  covering  tens  of  square  meters  to  composite  fail- 
ure zones  thousands  of  square  kilometers  in  area  and  from 
a  few  meters  to  hundreds  of  meters  thick  (Mcwre,  1961; 
Heezen  and  Drake,  1964;  Lewis,  1971;  Hampton  and 
Bouma,  1977). 

Subaqueous  mass  flows  involve  the  downslope  move- 
ment under  gravity  of  water-saturated,  unconsolidated 
sediment;  the  moving  mass  may  behave  plastically  or  as 
a  very  viscous  fluid,  and  movement  may  be  slow  or  rapid 
(Dott,  1963).  The  velocity  and  displacement  of  flow  char- 
acteristically decrease  gradually  with  depth  below  the  sur- 
face, so  that  the  deposit  lacks  a  distinct  slip  surface. 
Subaqueous  flow  deposits  are  identified  on  seismic-reflec- 


tion records  by  (I)  the  presence  of  anomalously  thick 
sediment  masses  apparently  detached  from  underlying 
strata,  (2)  the  absence  of  identifiable  slip  planes,  and  (3) 
acoustic  transparency  or  chaotic  internal  structure. 

Sediment  creep  in  the  marine  environment  is  a  form  of 
flow;  it  is  a  poorly  understood  and  poorly  documented 
phenomenon.  As  it  is  used  here,  sediment  creep  refers  to 
the  slow,  more-or-less  continuous  downslope  movement 
of  the  upper  layers  of  unconsolidated  sediment.  The  oc- 
currence of  creep  is  inferred  from  seismic-reflection  pro- 
files from  the  presence  of  hummocky  seafloor  top<igraphy, 
deformed  but  identifiable  acoustic  bedding  in  the  upper 
sediment  layers,  a  downward  decrease  in  the  degree  of 
deformation,  and  the  apparent  absence  of  a  slip  surface. 
Creep  may  extend  to  subbottom  depths  of  15-20  m,  is 
commonly  associated  with  other  types  of  failure,  and  may 
affect  large  areas. 


Hydrocarbons 

Natural  gas  of  biogenic  and  thermogenic  origin  may  be 
present  in  marine  sediment.  Biogenic  gas,  principally 
methane,  is  derived  from  bacterial  alteration  of  organic 
material  in  sediment.  Thermogenic  gas,  characterized  by 
relatively  high  levels  of  hydrocarbons  heavier  than  meth- 
ane, is  a  by-product  of  petroleum  formation.  The  presence 
of  thermogenic  gas  in  sediment  can  reflect  an  over-pres- 
surized zone  that  is  discharging  gas  into  the  overlying 
strata  via  a  conduit  such  as  a  fault  or  bedding  plane.  Gas 
of  either  type  present  as  bubbles  in  the  pore  space  of 
sediment  can  increase  pore  pressure  and  reduce  the  shear 
strength  of  the  enclosing  sediment,  and  thus  enhance  the 
likelihood  of  failure.  Under  some  circumstances,  sediment 
containing  dissolved  gas  can  liquefy  spontaneously  when 
it  is  subjected  to  cyclic  loading  such  as  may  be  imposed 
by  earthquake  shaking  (Hall  and  Ensiminger,  1979) 

Gas  accumulation  in  sediment  is  suggested  on  inter- 
mediate- to  high-resolution  seismic  records  by  ( 1 )  the 
presence  of  acoustic  amplitude  anomalies  (apparent  as 
enhanced  or  "bright"  subbtittom  reflectors),  (2)  the 
sharp  termination  or  displacement  of  reflectors  commonly 
a.ssociated  with  acoustically  turbid  zones,  (3)  the  absence 
of  surface  multiples  indicating  absorption  of  the  seismic 
signal  (Nelson  and  others,  1978),  and  (4)  the  presence  of 
"pull-downs,"  apparent  depressions  resulting  from  the  de- 
creased velocity  of  sound  in  ga.seous  sediment  and  conse- 
quent delayed  arrivals  of  acoustic  returns.  Water-column 
anomalies  on  high-resolution  seismic  records  in  some 
ca.ses  suggest  gas  bubbles  in  the  water  column,  although 
other  phenomena  such  as  kelp  and  fish  produce  similar 
appearing  features.  Side-scan  sonographs  and  underwater 
video  or  photographic  coverage  can  show  gas  seep 
mounds  or  gas-developed  craters  on  the  scaflo<ir.  Several 
lines  of  geophysical  evidence  are  desirable,  and  sampling 
and  gc(Khemical  analysis  are  needed  to  verify  the  presence 
of  gas  and  to  identify  its  origin. 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


EXPLANATION  OF 
STRATIGRAPHIC    TERMINOLOGY 
AND 
MAP  SYMBOLOGY 


Each  of  the  seven  maps  in  the  Cahfornia  continental 
margin  geologic  map  series  has  a  geologic  legend  and 
explanation  that  explains  the  symbols  and  terminology 
used  on  that  particular  map.  Here  we  have  presented  both 
a  legend  of  stratigraphic  units  and  unit  symbols  (see 
Master  Legend)  and  an  explanation  of  other  map  symbols 
(see  Master  Explanation)  that  are  comprehensive  in  their 
coverage  of  the  symbols  and  terminology  used  in  the  map 
series.  We  have  also  presented  examples  of  interpretive 
line  drawings  of  subbottom  profiles  (along  with  the  seis- 
mograms  on  which  they  are  based)  to  illustrate  the  use  of 
the  map  symbols  in  specific  geological  contexts. 


Stratigraphic  Units 

The  stratigraphic  units  used  in  this  study  are  lithostrati- 
graphic  in  nature.  In  most  cases,  an  age  or  age  range  is 
assigned  to  each  unit.  The  descriptions  and  the  age  desig- 
nations have  been  established  from  fairly  widespread  core, 
dredge  and  dart  samples  offshore  and  from  outcrops,  well 
logs  and  cores  in  the  immediate  onshore.  The  units  were 
then  correlated  across  large  regions  using  seismic  signal 
characteristics  that  differ  according  to  inherent  rock  prop- 
erties. These  units  can  be  referred  to  informally  as  "acous- 
tic stratigraphic"  or,  as  described  in  the  North  American 
Stratigraphic  Code  (code  of  stratigraphic  nomenclature), 
as  instrumentally  defined.  The  ages  should  be  considered 
part  of  the  general  description  of  each  unit,  and  the  reader 
should  be  aware  that  most  are  naturally  lime  transgressive 
or  regressive  in  nature. 

The  order  in  which  the  units  appear  is  approximately 
youngest  to  oldest,  but  this  order  should  not  be  looked 
upon  as  superpositional.  As  the  reader  will  quickly  dis- 
cern, many  of  the  units  given  in  the  Master  Legend  are 
local  in  extent. 


Geologic  Contacts 

Geologic  contacts  shown  on  the  maps  are  extrapolated 
from  a  combination  of  seismic-reflection  data,  samples, 
and  bathymetry,  and  are  approximate  in  location.  Unless 
otherwise  specified,  the  seafloor  geology  represented  on 
the  geologic  maps  is  covered  with  a  thin  (several  meters) 
layer  of  Quaternary  or  Holocene  sediments.  Thus,  the 
geologic  maps  represent  seafloor  geology  as  it  would  ap- 
pear if  the  thin  layer  of  Quaternary  sedimentary  cover 
were  removed.  Where  faults  offset  this  thin  layer  of  Qua- 
ternary sediments,  the  faults  are  given  the  age  symbol  for 
the  most  recent  sediments  they  cut,  even  though  they  are 
shown  on  the  map  as  existing  in  an  older  geologic  outcrop 
(for  example,  faults  of  Holocene  age  are  mapped  in  undif- 
ferentiated volcanic  and  sedimentary  rocks  of  Miocene 
age  on  the  top  of  Tanner  and  Cortez  bank. 

Symbols 

The  symbols  used  in  the  offshore  (see  Master  Explana- 
tion and  examples  1-46  of  subbottom  profiles)  to  denote 
specific  geologic  features  are  in  part  different  from  those 
traditionally  used  in  onshore  geologic  mapping.  This  dif- 
ference stems  from  the  data  acquisition  methods  used  in 
offshore  versus  onshore  mapping. 

Most  offshore  geologic  data  are  collected  by  remote 
sensing  techniques  that  yield  acoustic  seismograms  like 
those  shown  with  the  examples  of  subbottom  profiles. 
Many  of  the  examples  in  this  section  are  modified  from 
Greene  and  others  (1975,  1983)  and  Yerkes  and  others 
(1980).  Others  are  selected  from  data  collected  and  re- 
ported on  by  Kennedy  and  Welday  ( 1980),  Kennedy  and 
others  (1980),  Field  and  others  (1980),  Richmond  and 
others  (1981),  and  Clarke  and  others  (1983). 

Each  example  shows  a  short  reproduced  section  of  the 
seismic-reflection  profile  with  an  interpretive  line  drawing 
that  empasizes  a  particular  geologic  feature.  Beneath  each 
illustration  is  the  symbol  used  on  the  maps  and  a  short 
explanation  including  the  approximate  location  of  the  pro- 
file. All  features  considered  to  be  potential  geologic  haz- 
ards are  shown  in  red  on  the  geologic  maps.  Each  example 
has  a  number  which  is  keyed  to  a  location  map  (Figure 
2). 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


MASTER  LEGEND  OF 

(T""  Unconsolidated  deposits  of  Quaternary  age. 

Qf  Fan  deposits  of  Quaternary  age. 

Qd  Dellaic  deposits  of  Quaternary  age. 

Q/Qd  Deltaic  deposits  of  Quaternary  age  overlain  by 
thick  (greater  than  .^m)  deposits  of  Q. 

Qcf  Canyon  or  channel  fill  deposits  of  Quaternary 

age. 

Qt  Unconsolidated  marine  terrace  deposits  of  prob- 

able Pleistocene  age. 

Qp  Unconsolidated  marine  shelf  and  slope  deposits 

of  late  Pleistocene  age.      ^^^^- 

Qsp  Dcpt»its  that  may  correlate  with  the  San  Pedro 

Formation. 

Qar  Aromas    Red    Sands    (mostly    unconsolidated 

quartzose  sand  of  Pleistocene  age). 

Q/Qar  Aromas  Red  Sands  (mostly  unconsolidated 
quartzose  sand  of  Pleistocene  age)  overlain  by 
thick  (greater  than  3m)  dep<«its  of  Q. 

QTs  Sediment  and  sedimentary  rock  of  Quaternary 

-    •  and  Tertiary  (Pliocene  and  Miocene)  age. 

QTt  Terrace  deposits  of  Quaternary  and  late  Tertiary 

(?)  age. 

QTpr  Unconsolidated  sand,  gravel,  clay  and  tuff  of 

Pliocene  and  Pleistocene  age  that  may  correlate 
with  the  Paso  Robles  Formation. 

Q/QTpr  Unconsolidated  unit  of  sand,  gravel,  clay  and 
tuff  of  Pliocene  and  Pleistocene  age  that  may 
correlate  with  the  Paso  Robles  Formation,  and 
is  overlain  by  thick  (greater  than  .^m)  deposits 
of  Q. 


STRATIGRAPHIC  UNITS 

Tmv  Volcanic  rock  of  Miocene  ager 

Tmu  Volcanic  and  sedimentary  rocks  of  Miocene  age. 

TSC  Sania  Cruz  Mudstonc  (siliceous  organic  mud- 

stone  of  Miocene  age). 

Q/Tsc  Santa  Cruz  Mudstonc  (siliceous  organic  mud- 
stone  of  Miocene  age)  overlain  by  thick  (greater 
than  }m)  deposits  of  Q 


Tsm  Santa  Margarita  Formation  (sandstone  and  a'r- 

kosic  sandstone  of  Miocene  age). 

Q/Tsm  Santa  Margarita  Formation  (sandstone  and  ar- 
kosic  sandstone  of  MitKcne  age)  overlain  by 
thick  (greater  than  3m)  deposits  of  Q. 


Tp 

Sedimentary  rocks  of  Pliocene  age. 

Q/Tp 

Sedimentary  rocks  of  Pliocene  age  overlain  by 
thick  (greater  than  3m)  deposits  of  Q. 

Tpp 

Purisima  Formation  (marine  sandstone  and  silt- 
stone  of  Pliocene  age). 

0/Tpp 

Punsima  Formation  (marine  sandstone  and  silt- 
stonc  of  Pliocene  age)  overlain  by  thick  (greater 
than  3m)  deposits  of  Q. 

Tpr 

Sedimentary  rock  of  early  Pliocene  and  late  Mi- 
ocene age. 

Tm 

Sedimentary  rock  of  Miocene  age 

Q/Tm 

Sedimentary  rock  of  Miocene  age  overlain  by 
thick  (greater  than  3m)  deposits  of  Q. 

1 


Tmm  Monterey  Formation  (siliceous  sandstone,  silt- 

stone  and  mudstone  of  Miocene  age). 

Q/Tmm  Monterey  Formation  (siliceous  sandstone,  silt- 
stone  and  mudstonc  of  MiiKcne  age)  overlain  by 
thick  (greater  than  3m)  deposits  of  Q. 

Tmp  Plutonic  and  hypabyssal  rocks  of  Miocene  age. 

To  Sedimentary  rock  of  Oligocenc  age. 

Te  Sedimentary  rock  of  Eocene  age. 

Tep  Sedimentary  rock  of  Eocene  and  Paleocene  age. 

Tc  Carmelo  Formation  (sandstone,  siltstone,  mud- 

stone  and  cobble-pebble  conglomerate  of  Paleo- 
cene age). 

Ts  Sedimentary  rock  of  Tertiary  age. 

Tv  Volcanic  rock  of  Tertiary  age. 

Ku  Sedimentary  rock  of  late  Cretaceous  age. 

Kcs  Sedimentary  rock  of  Cretaceous  age. 

TMz  LinditTcrcntialed  igneous  nx-k  of  MuKcnc  age 

and   mclaniorphic  rock  of  pre-lale  Cretaceous 
age. 

Mz  Metamorphic  rock  of  pre-late  Cretaceous  age. 

gr  Granitic  rock,  chiefly  diorite,  of  Mesozoic  age. 

gdp  Porphyritic  granodiorite. 

m  Metamorphic  rock  of  unknown  age. 

Q/m  Metamorphic  rock  of  unknown  age  overlain  by 

thick  (greater  than  3m)  deposits  of  Q. 

KTc  Franciscan  Complex,  Coastal  Belt. 

KJf  Franciscan  Complex,  undirfcrentiated. 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


MASTER  LEGEND  OF  MAP  SYMBOLS 


GEOLOGIC  CONTACT:  Qucned  where  conuct  is  uncertain 
Contacts  are  extrapolated  from  seismic-reflection  data  and 
are  approximate  in  location. 


FAULTS:  Solid  where  well  defined,  dashed  where  approxi- 
mately located  or  inferred,  quened  where  uncertain.  Thrust 
fault  barbs  shown  on  upper  plate.  Where  fault  offsets  sea- 
floor,  age  symbol  is  shown  on  bar  on  downthrown  side. 
Elsewhere,  age  symbol  is  shown  astride  fault  and  relative 
offset  is  shown  by  "D"  and  "U"  on  downthrown  and  up- 
thrown  sides.  Ages  of  faults  are  indicated  as  follows: 


D 


T     T    ' 


■  Cuts  strata  of  Holocene  age. 

D  Cuts  strata  of  Pleistocene  age. 

B  Cuts  strata  of  Quaternary  age. 

O  Cuts  strata  of  late  Tertiary  and  Quaternary  age. 

A  Cuts  strata  of  Pliocene  age. 

A  Cuts  Miocene  or  older  strata. 

FAULT  ZONE 


FOLDS:  Solid  where  well  defined,  dashed  where  inferred,  que- 
ried where  uncertain.  Arrow  indicates  direction  of  axial 
plunge. 


Anticline 


Syncline 


FAULTED  ANTICLINE 


MAJOR  STRLCTLRAL  FEATURES 


StructuraJ  High 


0 
"6 


StructunJ  Low 


CHANNELS: 


Active:    Dash-dot  line  marks  axis,  arrow  indicates  direc- 
tion of  sediment  transport 


Filled:  Dash-dot  line  marks  axis,  arrow  indicates  direc- 
tion of  paleoscdiment  transport  Channel  boundary  solid 
where  well  defined,  dashed  where  inferred,  quened  where 
uncertain. 


Buried:  Dash-do(  line  marks  axis,  arrow  indicates  direc- 
tion of  paleoscdiment  transport  Channel  boundary  dotted, 
quened  where  inferred. 


LEVEES:     Solid  where  well  defined,  dashed  where  inferred, 
quened  where  uncertain 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


LANDSLIDES: 


Creep  (noted  on  single  survey  line);  Arrow  indicates  direc- 
tion of  sediment  movement. 


—i 


Creep  (area):  Solid  where  well  defined,  dashed  where  in- 
ferred, queried  where  uncertain. 


.4  TTITUDES: 


X 

Strike  and  dip  of  bedding. 
Apparent  strike  and  dip  of  bedding. 


DIAPIR:    Solid  where  well  defined,  dashed  where  inferred, 
queried  where  uncertain. 


GAS: 


Slump:  Solid  where  well  defined,  dashed  where  inferred, 
queried  where  uncenain.  Arrows  indicate  direction  of 
movement. 


^^^...TT^TrTTTTT.. 


■^TTT 


nr. 


Slump  scarp:     Solid  where  well  defined,  dashed  where  in- 
ferred, queried  where  uncertain. 


^jrw-irrn-irmt 


-n-?- 


Erosional  scarp:  Solid  where  well  defined,  dashed  where 
inferred,  queried  where  uncertain.  Generally  associated 
with  active  channels. 


I 

O I 

I 


Block  glide:  Solid  where  well  defined,  dashed  where  in- 
ferred, queried  where  uncertain.  Arrow  indicates  direction 
of  movement. 


Sediment  flow:  Solid  where  well  defined,  dashed  where 
inferred,  quened  where  uncertain.  Arrows  indicate  direc- 
tion of  movement. 


i 


Oil  and/or  gas  seep. 


Area  of  acoustic  anomaly  (possibly  indicating  trapped  shal- 
low gas) :  Solid  where  well  defined,  dashed  w here  inferred, 
queried  where  uncertain. 


2bnes  in  which  there  is  a  contmuous  gas-charged  reflector. 
Reflector  is  generally  shallow  (30  m)  and  lies  at,  or  near, 
the  base  of  the  unconsolidated  Quaternary  sediment. 


Zones  of  discontinuous  gas<harged  reflectors.  Reflectors 
lie  within  upper  Miocene  and  Pliocene  sedimentary  rock, 
and  within  unconsolidated  Quaternary  sediment. 


Area  of  shallow  subsurface  t:ontinuous  and  discontinuous 
gas  accumulation  within  Quaternary-  sediment.  Observed  on 
05-second  high-resolution  (Uniboom)  seismic  reflection 
profiles. 


Discontinuous  gas  accumulations  within  late  Tertiary-  and 
Quaternary  sedimentary  deptviits  Observed  along  individ- 
ual 2-sccond  intermediate-resolution  (air  gun)  seismic-re- 
Hcction  profiles. 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


Figure  2.  Location  mop  for  leiimic  profile  exomplei. 


1986 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


1.  GEOLOGIC  CONTACT  (buttress  unconformity) 


1950-  - 


KILOMETERS 


1960- 


GEOLOGIC  CONTACT:  queried  where  contoct  is  uncertain.  All  contoctj  are  extrapololed 
from  seismic-reflection  dofo  and  ore  opproximote  in  locotion.  Example  from  sparker  profile 
-?  of  upper  Tertiory  and  Quaternary  (QTs)  sediment,  ponded  in  synclinolly  folded  stroto  on 
slope  of  presumed  Miocene  (Tm?)  sediments.  Located  in  the  Gulf  of  Santo  Cotolino  west 
of  Dono  Point,  inner  southern  California  continental  borderland. 


10 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


2.  GEOLOGIC  CONTACT  (ponded  sediment) 


375 


450- 


q: 

u 

I- 

UJ 

2 


525 


600 


08 


0 
l_ 


05 


1.0 
I 


1.5 

—I 


KILOMETERS 


375 


0.5 


450- 


cr 
u 

»- 

UJ 

2 


525- 


600 


GEOLOGIC  CONTACT:  queried  where  contact  ij  uncertoin.  All  contacts  are  extrapolated 
from  seismic-reflection  data  and  are  opproximote  in  location.  Example  from  Uniboom  profile 
of  Quoternory  (Q)  sediment  ponded  in  synclinally  folded  Miocene  (TM)  sedimentary  rock. 
Located  south  of  San  Nicolos  Islond,  middle  southern  California  continental  borderland. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


11 


3.  GEOLOGIC  CONTACT  (ponded  sediment) 


638- 


713- 


cc 

LiJ 

u 

2 


TiTTT^TiTTuHflj, 


863 


-0  85 


788- f*- 


1 


05 

L_ 


10 

_J_ 


15 

_l 


KILOMETERS 


-095 


Q 

Z 

O 

u 

UJ 
to 


-1.05 


115 


638 


713- 


hi 

h- 
UJ 

2 


788- 


863 


0  85 


-0  95 


1/1 
Q 

Z 

o 
u 
liJ 

10 


-1.05 


115 


GEOLOGIC  CONTACT:  queried  where  contoci  is  uncertoin.  All  contocis  ore  extropoloted 
from  seismic-reflection  data  ond  are  approximate  in  location.  Example  from  Uniboom  profile 
of  unconsolidated  Quaternary  (Q)  sediment  ponded  between  base  of  slope  and  exposed 
bedrock  (?)  of  probable  Miocene  (TM?)  age  located  in  the  Gulf  of  Santa  Cotolino,  inner 
southern  California  continental  borderland. 


12 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


4.  FAULT  (seafloor  expression) 


1275 


0 

l_ 


_L 


2 


3 
_j 


KILOMETERS 


1125 


to 
q: 

u 

I- 
u 
2 


1200 


1275 


1. 


FAULT:  solid  where  well  defined,  dashed  where  inferred,  queried  where  uncertain.  Bar  and 
age  symbol  shown  on  downthrown  side  of  foulf  with  seafloor  expression.  Fault  displaces 
/  —  —  seafloor,  offsetting  acoustically  transparent  unit  (QTs)  of  presumed  late  Tertiary  and 
Quaternary  age.  Example  from  3.5  kHz  profile  across  inner  southern  Colifornia  continental 
borderland  near  San  Diego. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


13 


5.  FAULT  (seafloor  expression) 


188 


CO 

ct 

u 

UJ 

2 


263 


338 


•025 


0 

l_ 


0.5 

I 


1.0 

_J 


KILOMETERS 


188 


to 

»- 

UJ 

2 


263- 


338 


025 


035  1^0 
Q 

Z 

O 
u 

UJ 
lO 


045 


FAULT:  solid  where  well  defined,  dashed  where  inferred,  queried  where  uncertain.  Bar  and 
age  symbol  shown  on  downfhrown  side  of  fault  that  has  seafloor  expression.  Foult  displaces 
seofloor,  offsetting  sediments  of  presumed  late  Tertiary  and  Quaternary    (QTs)   age  and 

—  9 juxtoposing  subjacent  units  of  Miocene   (Tm)   and  possibly  Pliocene   (Tp?)   ages.  Also  note 

inferred  fault  within  probable  Miocene  section,  ond  folded  siralo.  Example  from  Uniboom 
profile  across  Tonner  Bank,  middle  southern  California  continental  borderland  (after  Greene 
and  others,   1975,  their  Figure  3). 


14 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


6.  FAULT  (seafloor  expression) 


KILOMETERS 


300 


600 


q: 


ui 

2  900 


1200- 


•04 


1. 


.08 


-V2 


I/) 
Q 

Z 

O 

u 

UI 


FAULT:  solid  where  well  defined,  dashed  where  inferred,  queried  where  uncertain.  Bar  and 
age  s/mbol  shown  on  downthrown  side  of  fault  that  has  seafloor  expression.  Fault  displaces 
seafloor,  offsetting  units  of  late  Tertiary  amd  Quoternory  (QTs)  age  and  juxtaposing 
subjacent  units  of  probable  Miocene  (Tm?)  age.  Example  from  sporker  profile  across 
mainland  shelf,  inner  southern  California  continental  borderland  near  Oceanside. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


15 


7.  FAULT  (seafloor  expression) 


1800 


KILOMETERS 


150C- 


1800-^ 


FAULT:  solid  where  well  defined,  dashed  where  inferred,  queried  where  uncertain.  Bar  and 
oge  symbol  shown  on  downthrown  side  of  foulf  that  has  seafloor  expression.  Divided  box 
indicates  youngest  strata  cut  are  of  Quaternary  age.  Note  that  one  questionable  and  four 

—  9 inferred  faults  cutting  Miocene  (Tm?)  or  older  strata  ore  indicated  by  open  triangles  astride 

foult  symbol.  "D"  designates  downthrown  block;  "U"  designates  upthrown  block.  The»e 
strata  are  also  folded,  as  shown  by  anticline  and  syncline  symbols.  Exomple  from  sporker 
profile  across  Gulf  of  Sonto  Catalina,  inner  sduthern  California  continentol  borderlond. 


16 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


8.  FAULT  (Quaternary) 


675- 


K 

Ul 

t- 

^825. 


975- 


•09 


I/) 

Q 

Z 

O 

-11    ^ 

I/) 


•  13 


J_ 


KILOMETERS 


675- 


^825. 


975. 


FAULT:  solid  where  well  defined,  dashed  where  inferred,  queried  where  uncertoin.  Faults 
designated  by  divided  boxes  indicote  that  strata  of  late  Tertiory  and  Quaternary  age  are 
cut.  One  of  these  has  seofloor  expression,  indicated  by  bar  ond  age  symbol  on  downthrown 
side;  another  reaches  but  does  not  displace  seofloor,  as  indicated  by  age  symbol  astride 
fault.  "D"  designotes  downthrown  block;  "U"  designates  upthrown  block.  Example  from 
sporker  profile  within  Lome  Seo  Valley,  inner  southern  California  continental  borderland. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


17 


9.  FAULT  (Tertiary) 


0 

i_ 


_L 


KILOMETERS 


450- 


-06 


525- 0-  — 


1/1 
a 

t- 

UJ 

2600" 


675- 


FAULT:  solid  where  well  defined,  doshed  where  inferred,  queried  where  uncertain.  Filled 
triangle    (oge  symbol)    indicates  youngest  strata  cut  are  Pliocene    (Tp)    in  oge.   Folded 

-p Miocene  (Tm)  sedimentary  rock  is  overlain  by  Pliocene  strato;  both  lie  in  fault  contact  with 

exposed  bedrock   ridge  of  folded  Miocene  strata.   Example  from  sporker  profile  across 
mainland  shelf  near  Carlsbad,  inner  southern  California  continental  borderland. 


18 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


10.  FAULT  (late  Tertiary  and  Quaternary) 


KILOMETERS 


FAULT:  solid  where  well  defined,  dashed  where  inferred,  queried  where  uncertain.  Divided 
box  astride  fault  symbol  indicates  fault  does  not  hove  seafloor  expression  ond  that  youngest 
strata  cut  are  of  lote  Tertiary  and  Quaternary    (QTs)    oge.  "D"  designates  downthrown 

9 block;   "U"   designates   upthrown   block.   Fault  extends  to  base  of   "bubble   pulse,"   but 

apparently  does  not  reach  the  seafloor.  Note  two  unconformities  within  strata  to  right  of 
foult.  Example  from  sporker  profile  across  inner  southern  California  continentol  borderland 
neor  Newport  Beach. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


19 


11.  FAULT  (late  Tertiarty  and  Quaternary) 


»y 


035 


KILOMETERS 


263 


•035 


56> 


FAULT:  solid  where  well  defined,  dashed  where  inferred,  queried  where  uncertoin.  Open 
circle  astride  fault  symbol  indicates  fault  does  not  have  seafloor  expression  and  that 
youngest  strata    (QTs)    cut  art  late  Tertiary  and  Quaternary  in  age.  Divided  box  astride 

Q  — "p fault   symbol   indicates   thof  the   strota  cut  are   undifferentiated   Quaternary   in  age.   "D" 

designates  downthrown  block;  "U"  designates  upthrown  block.  Fault  at  far  left  juxtaposes 
late  Tertiory  and  Quaternary  (QTs)  and  older  units  with  an  exposed  bedrock  ridge  of 
Miocene  (Tm)  rock.  Example  of  fault  zone  from  Uniboom  profile  across  San  Diego  shelf, 
Lomo  Sea  Valley,  and  Coronado  Bonk,  inner  southern  California  continental  borderland. 


20 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


12.  FAULT  (late  Tertiary  and  Quaternary) 


KILOMETERS 


-a— e- 


FAULT:  solid  where  well  defined,  dashed  where  inferred,  queried  where  uncertoin.  Open 
circles  astride  foult  symbol  indicotes  faults  do  not  hove  seafloor  expression  and  youngest 
strata  cut  are  late  Tertlory  and  Quaternory  (QTs)  in  oge.  "D"  designates  downfhrown 
block;  "U"  designates  upthrown  block.  Where  faults  ore  close  together,  they  ore  sometimes 
mapped  as  a  FAULT  ZONE  (see  Example  15) .  Note  that  fault  of  left  juxtoposes  late  Tertiary 
and  Quaternary  strata  with  on  exposed  bedrock  block  of  Miocene  (Tm)  age.  Example  from 
sparker  profile  ocross  Son  Diego  shelf,  Lomo  Sea  Volley,  and  east  flank  of  Coronodo  Bonk, 
inner  southern  California  continental  borderland. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


21 


13.  FAULT  (late  Tertiary  and  Quaternary) 


525- 


675- 


a: 
ui 

>- 

bJ 

5 


B25- 


975- 


-07 


-Q9 


>> 


Q 

Z 

o 
u 

UI 
in 


-13 


_1_ 


KILOMETERS 


525- 


675" 


in 

UJ 


825- 


975- 


-07 


-09 


1/) 
O 
z 
o 
u 

UJ 


-13 


FAULT:  solid  where  well  defined,  dashed  where  inferred,  queried  where  uncertain.  Open 
triangle  ostride  fault  symbol  indicates  foult  does  not  hove  seofloor  expression  and  strata 
cut  ore  probably  Miocene  (Tm?)  in  age.  "D"  designates  downthrown  block;  "U"  designotes 

-p  __  upthrown  block.  Note  also  the  two  faults  at  the  for  right  that  are  designated  by  filled  box 

and  bar  on  the  fault  symbol.  These  hove  seofloor  expression,  and  cut  strata  of  presumed 
Holocene  oge.  Example  from  sparker  profile  across  Son  Diego  shelf  to  Lomo  Sea  Valley, 
inner  southern  Colifornia  continental  borderland. 


22 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


14.  FAULT  (thrust) 


a/S- 


CO 

UJ 

I- 

UJ 


750- 


1125- 


1     ■'  Jv 


'••   •  .   ' 


.•?.«■    v^ 


-0.5 


C/3 
Q 

z 

o 
o 


-1.0 


-1.5 


2 

_l_ 


4 

J 


KILOMETERS 


375--. 


CO 

(E 
UJ 
H 
UJ 


1125- 


750- 


FAULT  (thrust) :  solid  where  well  defined,  dashed  where  inferred,  queried  where  uncertain. 

AAA -p Barbs  are  shown  on  upper  plate.  Note  thol  the  youngest  stroto  cut  ore  of  late  Tertiary  and 

Quoternory   (QTs)   age.  Example  from  sparker  profile  across  shelf  west  of  Ventura,  middle 
southern  California  continentol  borderland  (after  Greene  and  others,  1978,  their  Plate  1). 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


23 


15.  FAULT  ZONE 


w 

(E 
UJ 


0  ^ 


250 


500 


750 


W^ij^^^v: 


0.6 


^<-- 


1-r- 


•i^-' 


.^.0.4 


0.2 


Q 

Z 

o 
o 

UJ 

w 


0.5 

I 


1  .0 


KILOMETERS 


0 


250 


CO 

cr 

UJ 

h- 
UJ 


500 


750 


QTs 


f^\w\^i 


o.e 


0.8 


10 


^^  ^^ FAULT  ZONE:  jolid  where  well  defined,  dashed  where  inferred,  queried  where  uncerfoin 

,W^N^^N^^     Fault  zone  offietj  jedimenlory  rockj  of  Miocene   (Tm)   oge  ond  locally  moy  extend  to  the 
Vv>VV>\\\\\N     seafloor.  Exomple  from  the  sparker  profile  across  shelf  south  of  San  Moteo  Point,  inner 
southern  Colifornio  continental  borderlond    (after  Greene  and  Kennedy,   1981). 


24 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


16.  FAULTED  ANTICLINE 


C/3 

cr 

I- 

LU 


375 


750 


=  -0.5 


CO 

o 
z 
o 
o 

UJ 
CO 


1.0 


0         1         2 
I I I 

KILOMETERS 


CO 
QC 
LU 

H      375  H 
LU 


750  - 


-0.5 


CO 

D 

Z 

o 
o 

LU 
CO 


-  1.0 


FAULTED  ANTICLINE:  Gas  migrating  upward  along  faults  in  late  Tertiory  and  Quaternary 
(QTs)  strota  has  accumuloted  along  the  foulted  anticlinol  crest,  increasing  the  acoustic 
contrast.  Example  from  2-sec,  single-channel  oirgun  reflection  record  in  offshore  Santa  Mario 
basin,  south  central  California  continental  margin. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


25 


17.  FOLD  (anticline) 


150-r 


0.2 


225- 


UJ 

I- 

1 


300- 


375 


0 

L 


■1-0.5 


0.25 

I 


05 

_J 


KILOMETERS 


150 


225- 


q: 

u 

I- 

UJ 

2 


300- 


375 


0.2 


-0.3 


O 

z 
O 

CO 


-0.4 


0.5 


-?  — 


FOLD  (anticline):  oxis  shown  os  lolid  line  where  well  defined,  daihed  where  inferred, 
queried  where  uncertain.  Arrow  indicates  direction  of  oxial  plunge.  Also  note  small  syncline 
to  right  of  anticline,  and  ongulor  unconformity  between  undifferentiated  igneous  and  sedi- 
mentary rocks  of  proboble  Miocene  age  (Tmu?) ,  and  overlying  stroto  of  Miocene  (Tm)  oge. 
Example  from  Uniboom  profile  between  the  Tanner  end  Cortes  Banks,  middle  southern 
California  continentol  borderland. 


26 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


375- 


450- 


q: 
lij 

I- 

Ui 

2 


525 


18.  FOLD  (anticline,  syncline) 


-rv  :  ^).6 


600 


-05 


Q 

Z 

o 

u 

Ixl 

to 


-0  7 


0.8 


KILOMETERS 


375- 


450- 


q: 

u 

I- 


525- 


600 


-? 


FOLD  (anticline):  axis  shown  as  solid  line  where  well  defined,  dashed  where  inferred, 
queried  where  uncertain.  Arrow  indicates  direction  of  axial  plunge.  Also  note  small  syncline 
locoted  between  the  two  onticlinol  folds,  ond  the  angulor  unconformity  between  folded 
stroto  of  Miocene  (Tm)  age  and  the  progradofionol  sequence  of  Miocene  (Tm)  sedimen- 
tary rocks.  Example  from  Uniboom  profile  across  San  Nicolas  Island  platform,  middle 
southern  Californiti  continental  borderland. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


27 


19.  STRUCTURAL  HIGH  AND  LOW 


CO 
Q 

z 
o 
o 
m 

CO 


0 


10 

_J 


20 

—I 


KILOMETERS 


2250 


QTs 


gr 


-0 


-1 


-2 


-3 


CO 
Q 

z 
O 

o 

UJ 
CO 


0 

~6 


STRUCTURAL  HIGHS  AND  LOWS:  solid  where  well  defined,  doshed  where  inferred. 
Structurol  highs  formed  by  the  Forallon  Ridge  (Crefoceous  granitic  rocks,  gr,  of  the  Salinion 
ferrone  of  Siberling  and  others,  1984)  and  the  Santo  Cruz  high  (Cretoceous  subduction 
melange  of  Franciscon  Complex,  KJf )  and  the  intervening  structural  low  filled  by  late  Terliory 
and  Quaternary  sediments  of  the  outer  Santo  Cruz  basin.  Line  drawing  from  a  4.second, 
single-channel  sparker  profile  run  across  the  continental  shelf  and  slope  west  of  Half  Moon 
Bay,  offshore  centrol  Colifornio. 


28 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


20.  STRUCTURAL  HIGH 


aTS' 


0  5 


0 

1_ 


I 


KILOMETERS 


375- 


450- 


K 

UJ 

l- 
UJ 

2 


525-^^ 


600- 


675- 


V 


\ 


-05 


-09 


STRUCTURAL  HIGH:  solid  where  well  defined,  dashed  where  inferred.  Top  of  structural  high 
is  surface  eroded  onto  presumed  sedimentary  rocks  (Ts)  of  Tertiary  age  buried  beneoth 
undifferentioled  sedimentary  rocks  and  sediments  (QTs)  of  Tertiary  and  Quaternary  age. 
Example  from  sparker  profile  across  the  Gulf  of  Santo  Catalino. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


29 


21.  CHANNEL  (active) 


300- 


00  600- 
UJ 

I- 

UJ 

2  900- 


1200- 


1500- 


^20 


O       1 
I L 


3       4 
_l L 


KILOMETERS 


300- 


(/)600- 
UJ 


1200- 


1500- 


i 


i 


i 


buried 
channels 


—0.4 


-0 


■20 


Channel  (octlve) :  da$h-dot  line  morks  chonnel  oxij,  arrow  indicates  direction  of  sediment 
transport.  Also  note  two  buried  channels  beneoth  the  modern  seofloor  of  presumed  Quoter- 
nory-Tertiory,  undifferentioted  age  to  right  of  active  channels.  Example  from  sparker  profile 
across  head  of  Arguello  Canyon,  off  Point  Arguello,  central  Coiifornia  continental  margin. 


30 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


22.  CHANNEL  (filled) 


75- 


2 


150- 


225- 


■HUU 


-01 


to 
Q 

z 
O 
u 

UJ 

if) 


KILOMETERS 


to 

UJ 


to 

Q 

2 

o 
u 

to 


150- : 


225 


5G5fil^^i^ 


CHANNEL  (filled):  dosh-dot  line  marks  poleochonnel  oxis,  arrow  indicates  direction  of 
sediment  transport.  Channel  margins  indicated  by  solid  line  where  well  defined,  doshed 
where  inferred,  queried  where  uncertain.  Also  note  fault  thot  cuts  flat  lying  sediments  of 
presumed  Holocene  age  and  is  expressed  in  the  seafloor.  Example  from  Uniboom  profile  off 
Point  Ano  Nuevo,  centrol  California  continental  margin. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


31 


23.  CHANNEL  (filled) 


'    ■'!      \' 


»■  ■!  gill  i 


{fPSilin^Tf*^ 


0 

i_ 


0  25 

I 


050 
I 


(•♦>» 


.0.45 


I/) 
Q 

-0.55    g 

U 
Ul 

10 


-0.65 


KILOMETERS 


338. 


[iJ   413' 

UJ 

1 


488- 


-0.65 


5S5ai^.5©SS 


CHANNEL  (filled) :  dath-dot  line  markj  poleochannel  axis,  arrow  indicates  direction  of 
sediment  transport.  Channel  margins  indicoted  by  solid  line  where  well  defined,  dashed 
where  inferred,  queried  where  uncertain.  Example  from  Uniboom  profile  of  upper  Tertiary 
and  Quaternary  (QTs)  sediments  filling  an  erosional  chonnel  locoted  off  Point  Lo  Jollo,  inner 
southern  California  continentol  borderland. 


32 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


24.  CHANNEL  (filled) 


637-  --ir 


(/5  712- 
q: 

Hi 

u 


787- 


862- 


-085 


rP 


-095  S 

z 
O 


-1.05 


•115 


05 


1.0 


15 


KILOMETERS 


637- 


U)  712- 
UJ 

2 


787- 


862- 


\      ,/ 


-1.15 


•-V 


5fe 


CHANNEL  (filled):  dash-dot  line  marks  paleochannel  axis  (not  located  on  profile  above), 
arrow  indicates  direction  of  sediment  transport.  Channel  margins  indicated  by  solid  line 
where  well  defined,  dashed  where  inferred,  queried  where  uncertain.  Note  that  old  channel 
deposits  (Qcf)  have  been  incised  b/  subsequent  erosion,  resulting  in  the  formation  of  a 
modern,  active  channel.  Symbols:  QTs,  upper  Tertiary  and  Quaternary  sediments;  Tpp?, 
Pliocene  Purisimo  (?)  Formation.  Example  from  Uniboom  profile  across  Ascension  Canyon, 
central  Colifornio  continental  margin. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


33 


25.  CHANNEL  (buried) 


450 


750- 


i/i 
cr 

UJ 

5 


1050 


1350 


0 

L- 


X 


KILOMETERS 


450- 


750- 


r^^y^A 


y^ 


-0  6 


•10 


-14 


CO 
O 

z 
O 
u 
liJ 


-18 


.\^.\« 


CHANNEL  (buried):  dash-dot  line  morkj  poleochonnel  oxis,  orrow  indicates  direction  of 
sediment  transport.  Channel  margins  indicated  by  dotted  line.  Also  note  the  chonnel  ot 
surfoce,  above  ond  to  the  left  of  buried  channel,  filled  with  undifferentiated  sediments  of 
lote  Tertiary  and  Quaternary  (QTs)  age.  A  modern  channel  occupying  the  site  of  this  older, 
filled  chonnel  may  be  indicoted  by  the  presence  of  low-relief  erosionol  scarps  at  the  surfoce. 
Example  from  sparker  profile  across  the  Gulf  of  Santo  Catolino,  off  Dono  Point,  inner 
southern  California  continental  borderland. 


34 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


26.  CHANNEL  (buried) 


1500- 


101  IIIB  iJ 

«i    ft     exec 


^^^^-^iT^iUt:  i-^^^-^' 


KILOMETERS 


1500- 


,V^\ 


CHANNEL  (buried):  dojh-dot  line  marks  paleochannel  axis  (not  indicated  on  profile 
above)  .  Within  upper  Tertiory  and  Quaternary  (QTs)  sediments,  the  channel  margins  are 
indicated  by  dotted  lines.  Pulled-down  reflectors  immediately  beneath  the  channel  and 
incoherent  reflectors  at  depth  probably  result  from  low  acoustic  velocities  ossocioted  with 
unconsolidated  channel  fill  materials.  Example  from  sporker  profile  across  the  Gulf  of  Santa 
Catalina,  inner  southern  California  continental  borderland. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


35 


27.  LEVEE 


150- 


450- 


tr 

h- 

LU 


750- 


1050- 


— 55^^ 


-  .6 


I'      i       'Tr<''s  Tra-Tri.-ti'.-'ji  [..■gQiys  ■■!!-.   vsrrriKTHsrrz 


--.-3:^ 


;:-t::::ipi 


■T'^' 


11:1 


CO 

Q 

z 
O 
o 

LU 
CO 


-  1.4 


J 


KILOMETERS 


150- 


450- 


1050- 


-  .6 


LEVEE:  solid  where  well  defined,  dashed  where  inferred,  queried  where  uncerfoin.  Levees 
constructed  from  sediment  overflow  of  active  submorine  channel  (shown  os  doshdot  line 
with  orrow  indicating  direction  of  sediment  transport)  .  Levees  of  Quaternary  age  ore 
deposited  upon  flat  lying  strata  of  sediments  and  sedimentary  rocks  of  Quaternory  and 
Tertiary,  undifferentiated,  oge  (QTs).  Example  from  sparker  profile  across  floor  of  Gulf  of 
Santa  Cotolina  at  base  of  slope  west  of  Son  Mateo  Point,  southern  California  continental 
borderland. 


36 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


28.  LANDSLIDE  (creep) 


563- 


638- 


q: 
u 

I- 

UJ 

2 


713- 


-085 


■075 


O 

z 
O 
u 

UJ 

I/) 


-095 


788- 


i, 


05 


0 


0.5 

l_ 


10 

L_ 


15 
I 


KILOMETERS 


563 


638- 


u 

u 

2 


713- 


788 


075 


-085 


1/5 

Q 

Z 

O 
U 
UJ 
10 


-095 


105 


CREEP  (noted  on  o  single  survey  line)  :  orrow  indicates  opparent  direction  of  sediment 
movement  in  upper  Tertiary  ond  Quoternary  (QTs)  sediments.  Example  from  Uniboom 
profile  off  Oceonside,  inner  southern  California  continental  borderland. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


37 


29.  LANDSLIDE  (slump) 


563- 


O 

l_ 


_L 


2 
-I I 


-075 


KILOMETERS 


563- 


788- 


075 


-085 


I/) 
O 


k095  uj 


-105 


-9  — 


SLUMP:  boundaries  solid  where  well  defined,  dashed  where  inferred,  queried  where  uncer- 
tain. Arrows  indicate  direction  of  movement.  Zone  of  movement  extends  to  a  subbottom 
depth  of  opproximotely  20  m.  Note  hummocky  seafloor  surfoce  and  back-rotated  subbottom 
reflectors  (slip  surface)  .  Exomple  from  Uniboom  profile  across  continentol  slope  off  Crescent 
City,  northern  California  continental  margin. 


38 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


30.  LANDSLIDE  (slump) 


375' 


KILOMETERS 


375' 


SLUMP:  boundaries  solid  where  well  defined,  dashed  where  inferred,  queried  where  uncer- 
tain. Arrows  indicate  direction  of  movement.  Zone  of  movement  extends  to  a  subbottom 
depth  of  30  m.  Note  hummocky  seafloor  surface,  slip  surfoces  and  bock  rotation  of  reflectors 
within  moving  sediment  moss.  Exomple  from  Uniboom  profile  across  slope  west-northwest 
of  Crescent  City,  northern  California  continental  morgin  (after  Field  and  others,  1980,  their 
Figure   15) . 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


39 


31.  LANDSLIDE  (slump) 


-0.35 


KILOMETERS 


-035 


-045 


563 


— '?— ^ 


-055 


-065 


075 


SLUMP:  boundaries  solid  where  well  defined,  doshed  where  inferred,  queried  where  uncer- 
tain. Arrows  indicate  direction  of  movement.  Zone  of  movement  extends  to  o  subbottom 
depth  of  in  excess  of  100  m  involving  sediments  of  late  Tertiory  and  Quaternary  (QTs)  age. 
Note  slip  surfaces  and  apparent  drag  folding  of  strato  adjacent  to  slip  surfoces.  Example 
from  Uniboom  profile  neor  La  Jolla  Conyon,  inner  southern  California  continental  border- 
land. 


40 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


32.  LANDSLIDE  (slump) 


150- 


225- 


liJ 

2 


300- 


375- 


T-02 


KILOMETERS 


150-r 


225- 


a: 

UJ 

1 


300- 


375 


SLUMP:  boundaries  solid  where  well  defined,  dashed  where  inferred,  queried  where  uncer- 
tain. Arrows  indicate  direction  of  movement.  Zone  of  movement  extends  to  a  subbottom 
depth  of  approximately  90  m  in  sediments  of  late  Tertiary  and  Quoternory  (QTs)  age.  Note 
apparent  slip  surfaces  and  bock-rotated  reflectors.  Exomple  from  Uniboom  profile  across 
Ascension  Canyon,  central  California  continental  margin. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


41 


33.  LANDSLIDE  (slump) 


0-'  r—l  >- 


80- 


«       100- 


150- 


200- 


T  ^r,^;.  ,■•/•. i■"y^^l^^;^-;i^^;:*•^  t i'i^j. if -r  I  -iin'-T^!;"    jV"''  i.T-ri;  ..■"*";'" "° 


^^^^   ■'■■'"■!;' -iCiii'^i?!' ;';•;;; "li 


-005 


(A 

-0  10     o 

O 
<j 


-0  15 


-0.20 


0.5 

_J 


1 


1.5 

-I 


KILOMETERS 


0  — 


50- 


100- 


150- 


200- 


—  9 . 


SLUMP:  boundaries  solid  where  well  defined,  dashed  where  inferred,  queried  where  un- 
certain. Arrows  indicate  apparent  direction  of  movement  in  deposits  of  late  Tertiary  and 
Quoternory  (QTs)  age.  Movement  of  the  slump  mass  along  a  generally  arcuate  failure 
surface  has  destroyed  the  bedding  and  produced  o  nonreflecling  zone.  Example  from 
Uniboom  profile  across  the  continentol  slope  off  outer  Santa  Cruz  bosin,  central  Californio 
continental  margin. 


42 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


34.  LANDSLIDE  (scarps) 


375 


1-05 


675 


0                    1                    2 
I I 1 I 1 

KILOMETERS 


375 


450- 


q: 


t^525- 


600-  : 


675 


^^rmrrmrr.- 


■^TTT; 


SCARPS:  boundoriej  solid  where  well  defined,  doshed  where  inferred,  queried  where 
uncerfoin.  Hochures  indicote  slump  scorp.  Zone  of  movement  involves  sediment  of  late 
Tertiory  and  Quaternary  (QTs)  oge.  Note  double  hochures  indicate  erosionol  scarps. 
Example  from  Uniboom  profile  ocross  La  Jolla  Canyon,  inner  southern  Colifornio  contlnentol 
borderland. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


43 


35.  LANDSLIDE  (block  glide) 


450-1 


750-  ; 


I/) 
q: 

UJ 
Ul 


1050- 


1350- 


-0.6 


KILOMETERS 


450- 


750- 


I/) 
a: 

UJ 

h- 
UJ 


l<3- 


QTs 


1-06 


QTs 


1050- 


Tm? 


1350- 


•10 


1/1 
Q 

z 
O 
u 

Ul 


.14 


-?--! 


BLOCK  GLIDE:  boundaries  solid  where  well  defined,  dashed  where  inferred,  queried  where 
uncertain.  Arrows  indicate  opporenf  direction  of  movement  Zone  of  movement  extends  to 
a  subbotfom  depth  of  150- 190  m,  involving  sediments  of  late  Tertiary  and  Quaternory 
(QTs)  age.  Note  relative  acoustic  transparency  of  blocks,  possibly  the  result  of  intense 
deformation  of  strata  within  the  blocks.  Erosional  channels  may  develop  locally  along 
pull-apart  fractures  between  blocks,  shown  by  double  hachures  (erosional  scorp)  .  Example 
from  sparker  profile  across  base  of  slope  off  Newport  Beach,  inner  southern  California 
continental  borderland   (after  Greene  and  others,  1983,  their  Figure  2-10). 


44 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


36.  LANDSLIDE  (block  glide) 


i 

1 

Af^Ci^ 

^ 

k 

Mm 

"06 

M 

■ 

!! 

^ 

AL 

'JiL 

M 

.   1 

V.vt 

'^i/i  ■•- 

10  525" 

01 

•^/?k*»«^.  . 

t 

■07 

LiJ 

1- 
iii 

■lk->..^^ 

r 

mmsrsf 

z 

W 

:     "'! 

t::.        .               -"m^'M.    r^.     %^^ 

"^ 

^^^ 

n|Hi 

-ym-i^ 

-9 

f^r\r\^ 

•'-^ 

'  / 

k 

' ' 

\^ 

s 

k 

*l^ 

■ 

i^'f 

•* 

0 

L_ 


KILOMETERS 


600- 


675- 


-06 


-0  9 


■-?--! 


BLOCK  GLIDE:  boundaries  solid  where  well  defined,  doshed  where  inferred,  queried  where 
uncertain.  Arrows  indicate  apparent  direction  of  movement.  Zone  of  movement  extends  to 
a  subbottom  depth  of  approximately  90-100  m,  involving  sediments  of  late  Tertiary  and 
Quaternary  (QTs)  age.  Note  that  internal  deformation  of  blocks  is  greatest  toward  the  front 
edge  (downslope),  and  sole  (base)  of  the  mass.  Locally,  erosional  channels  may  develop 
along  pull-opart  fractures  between  the  blocks.  These  ore  shown  with  double  hochures 
(erosional  scarp) .  Example  from  mini-sparker  profile  across  slope  south  of  Newport  Beach, 
inner  southern  Colifornio  continental  borderland. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


45 


37.  LANDSLIDE  (sediment  flow) 


225- 


w 

liJ 

I- 
liJ 

2 


300- 


375- 


•■} ',; 


T-   frfTfr*  I   ■■:■;     '■  .    I  '  !    ■'!■  !'A '■■•:;■,    (    iv 
.  •     1»  ir .?.' -^  ..'.  :v  :  ■.  I  ;•  •!.    r'    't  ■     '    . 


I    -(5 


0.3 


0.5 


1.0 

—I 


KILOMETERS 


225- 


LLI 

2 


300- 


375- 


1.  •.■  .■•.•■i'.'-'-v  ■..■•.:  ■;•••>■•. 


..rV^;.r>->.x^.v.-' 


-0.5 


•i."i»!K:-';) 


SEDIMENT  FLOW:  Boundaries  solid  where  well  defined,  dashed  where  inferred,  queried 
where  uncertain.  Arrows  indicate  direction  of  movement  in  sediments  of  lofe  Tertiory  ond 
Quaternary  (QTs)  age.  Note  multiple  headscarps  obove  thick,  detached  sediment  moss, 
acoustic  transparency  of  this  mass,  and  absence  of  an  identifiable  slip  surfoce.  Example  from 
Uniboom  profile  across  north  slope  of  Santo  Barbara  Channel,  (approximately  35  km)  west 
of  Santo  Borboro    (from  Edwards,   1982). 


46 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


38.  GAS  (seep) 


375 


450- 


q: 

UJ 

I- 

UJ 

I. 


525- 


600 


T^O.5 


-0.6 


I/) 
Q 
z 
O 
u 
u 


-.-O? 


0 


0.5 

I 


10 


1.5 

_i 


KILOMETERS 


08 


375 


450- 


q: 

u 

t- 

UJ 

2 


525- 


600 


0.5 


-0.6 


z 
O 
u 


-07 


08 


I 


OIL  AND/OR  GAS  SEEP:  symbol  indicates  presence  of  subbotfom  ond  water  column 
ocoustic  anomalies  associated  with  gas  seeps.  Gas  seep  occurs  in  sediments  of  late  Tertiory 
ond  Quaternary  (QTs)  oge.  Queried  where  uncertain.  Example  from  Uniboom  profile  across 
base  of  slope  off  Point  La  Jolla,  inner  southern  California  continental  borderlond  (after 
Greene  ond  others,  1983,  their  Figure  2-16). 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


47 


39.  GAS  (bright  spot,  subsurface) 


75- 


150 


225 


KILOMETERS 


225 


GAS:  area  of  acouttic  anomaly,  possibly  indicating  the  presence  of  gas-saturated  sedi- 
ments. Solid  where  well  defined,  dashed  where  inferred,  queried  where  uncertain.  Acoustic 
anomalies  above  occur  in  flat-lying  Quaternary  (Q)  sediment  overlying  an  eroded,  flat- 
topped,  Miocene  (Tm)  bedrock  ridge.  Exomple  from  Uniboom  profile  across  San  Pedro 
escarpment  and  shelf,  middle  southern  California  continentol  borderland. 


48 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


40.  GAS  (bright  spot,  subsurface) 


150 


10 
K 
(iJ 

I- 
lU 


225- 


300 


0 
I 


Jte04 


KILOMETERS 


150- 


UJ 

I- 
2 


O 

z 
O 
u 

UJ 


225- 


300 


GAS:  area  of  acoustic  anomaly,  possibly  indicating  the  presence  of  gos-saturoted  sediment. 
Solid  where  well  defined,  dashed  where  inferred,  queried  where  uncertoin.  Example  from 
Uniboom  profile  across  shelf  and  upper  slope  west  of  Crescent  City,  northern  California 
continental  margin. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


49 


41.  GAS  (bright  spot,  subsurface) 


0 

i_ 


_i_ 


KILOMETERS 


GAS:  area  of  acoustic  anomaly,  possibly  indicating  the  presence  of  gas  saturated  sediment. 
Solid  where  well  defined,  dashed  where  inferred,  queried  where  uncertain.  Example  from 
3.5  kHz  profile  across  shelf  off  Crescent  City,  northern  California  continental  margin. 


so 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


42.  DIAPIRIC  RIDGE 


250 


033 


KILOMETERS 


250 


0  33 


-?— . 


DIAPIRIC  RIDGE:  Solid  where  well  defined,  doshed  where  inferred,  queried  where  uncertain. 
Shale-cored  diapir  pierces  upper  Tertiary  and  Quoternary  (QTs)  strata  ond  extends  above 
the  seafloor.  Example  from  3.5  kHz  profile  across  marginal  plateau  west-northwest  of  Eureka, 
northern  Colifornio  continental  margin. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


51 


43.  DIAPIRIC  RIDGE 


1500 


0 


4 

_l 


KILOMETERS 


300- 


600- 


q: 

UJ 

^  900H 


1200- 


1500- 


DIAPIRIC  RIDGE:  Solid  where  well  defined,  dashed  where  inferred,  queried  where  uncertoin. 
Shole-cored  diopir  pierces  upper  Tertiary  and  Quaternary  (QTs)  and  older  strata  ond 
extends  obove  the  seafloor.  Example  from  sporker  profile  across  morginol  plateau  west- 
northwest  of  Eureka,  northern  California  continental  margin. 


52 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


44.  TERRACE  (constructional) 


I' p  rr»pm:'ii^)a!.m:  ;y:;t-    ;- ;  ■     ly-r  '■.^■'jri  ~  ^m9^»'^f.lm^fn■:"'^Ffr'Wf^^^   •'■' 


75- 


I 


•9!ra 


1 


v> 

Ul 


•-150-  -= 


225 


3O0- 


05 

I 


10 


KILOMETERS 


75- 


q: 
ui 


^-150- 


225- 


3O0- 


-01 


■04 


TERRACE  (constructional) :  Example  from  Uniboom  profile  across  east  flank  of  Cortes  Bonit, 
middle  southern  Colifornio  continentol  borderland,  showing  Pleistocene  (QT)  progrodotion- 
al  terroce  sequences  forming  a  constructional  or  depositional  marine  terrace  (after  Greene 
and  others,  1975,  their  Figure  5). 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


53 


45.  TERRACE  (erosional) 


KILOMETERS 


75- 


1/1 


tu 

2 


225" 


300" 


acousticolly   tronsporent  unit 


angular    unconformity 


-01 


I-02S 

z 
O 

(/) 


-03 


-04 


TERRACE   (erosional):  Example  from  Uniboom  profile  ocross  shelf  off  Point  La  Jolla,  inner 
southern  Colifornio  continental  borderland.  Undifferentiated,  folded  Cretaceous  strota  (Ku) 
ond  overlying  upper  Tertiary  and  Quoternary    (QTs)    progradotionol  sequence  hove  been 
bevelled  by  wave  action.  Acoustically  Ironsporonf  unit  overlying  wove-cut  platform  is  proba 
biy  Holocene   (Q)    in  age. 


54 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


46.  TERRACE  (erosional) 


150 


-0.1 


00 
Q 

Z 

O 
u 


_. L 


KILOMETERS 


75- 

CO 

cc 

UJ 

\- 

LlI 

150- 


-0.1 


00 
Q 

Z 

O 
u 

Ld 

00 


•0  2 


TERRACE  (erosionol):  Wove-ploned,  platform  composed  of  undifferentioted,  folded  Crefo- 
ceoui  (Ku)  strato,  forming  o  wove-cul  terrace,  partially  overlain  by  acoustically  transporont 
layer  of  Holocene  (Q)  age.  Example  from  Uniboom  profile  across  shelf  off  Point  La  Jolla, 
inner  southern  California  continental  borderland  (ofter  Greene  and  others,  1983,  their 
Figure  2-18). 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


55 


COMPOSITE  STRATIGRAPHIC  SECTIONS 

The  stratigraphic  columns  are  composite,  generalized 
sections  developed  by  compiling  and  modifying  onshore 
and  offshore  data  from  Greene  and  Clark  ( 1*)79),  Hoskins 
andGrifTiths  (1971),  Howell  and  others  (1978),  McCul- 
loch  and  others  (1982.  1985),  Vedder  and  others  ( 1974, 
1976,  1980),  and  Clarke  (1987),  as  well  as  from  unpub- 
lished sources. 

Each  of  the  columns  shows  the  generalized  geology  for 
the  area  in  which  it  is  located.  Each  section  has  a  number 
that  is  keyed  to  a  location  map  (Figure  3).  The  reader 
should  not  attempt  to  correlate  the  stratigraphic  units 
from  the  columns  to  the  maps  because  the  maps  are  con- 
structed primarily  from  acoustic  stratigraphic  units  and 
the  columns  represent  rock  stratigraphic  units  exclusively. 
Rock  stratigraphic  names  are  tentatively  correlated  to 
acoustic  units  on  the  geologic  legends  only  where  dredge 
and  core  data  support  their  use.  The  thickness  of  geologic 
units  shown  on  the  columns  is  approximate  and  was 
derived,  where  available,  from  seismic  velocities,  well  logs, 
and  onshore  geologic  maps. 

The  reader  should  note  that  the  diagramatic  strati- 
graphic columns  from  Hoskins  and  Griffiths  (1971)  in- 
cluded in  the  text  are  not  individual  well  sections,  but  are 
composite  representative  sections  for  entire  offshore  ba- 
sins, and  that  the  indicated  thicknesses  are  the  interval 
maximum  for  the  entire  basin. 


Figure  3 
Areas 

1.  Eel  River  Bosin  I 

2.  Point  Areno  Bojin    B 

3.  Bodega  Bosin  B 

4.  Outer  Santo  Cruz  Basin    B 

5.  N.  Monterey  Bay  Region  A 

6.  S.  Monterey  Boy  Region    A 

7.  OHshore  Santo  Mario  Bosin  B 

8.  N.  Santo  Borboro  Chonnel    E 

(OCSCAL  78164  No.  1) 

9.  Santo  Ynez  Unit  and  vicinity  C,G 

10.  Dos  Cuadros  oilfield  and  vicinity    G,H 

11.  Son  Miguel  Island    F 

12.  Sonto  Rosa  Island    F 

13.  Sonfa  Crui  Island    F 

14.  N.E.  Coast  Santo  Cruz  Island  C,G 

15.  OHshore  Santo  Monica  Bosin  C,G 

16.  N.  Santo  Roso  -  Cortes  Ridge  C,G 

17.  Northern  Potion  Ridge  C,G 

18.  Sonto  Cruz  •  Catolino  Rid0«  C,G 

19.  Son  Pedro  Bosin  C,G 

20.  Newport  Beach      Dona  Pf.  SheK    C,G 

21.  Sonto  Cotolino  Island    F 

22.  Son  Nicolas  Island  F 

23.  Son  Clemente  Ridge    C,G 

24.  S.  Gulf  of  Sonto  Catolino  C,G 

25.  Son  Clemente  Island    G 


26.  Son  Nicolas  Basin    C,G 

27.  Doll  Bonk   C,G 

28.  Thirtymile  Bonk    C,G 

29.  Son  Diego  Shelf C,G 

30.  Fortymile  Bank   C,G 

31.  Centrol  Bloke  Knolls  C,G 

32.  Cortes  Bonk    C,G 

(OCSCAL  75-70  No.  1) 

33.  Northeast  Bonk    C,G 


Figure  3 
References 

A. —  Greene,  H.G.,  ond  Clork,  J.C,  1979,  Neogene  poleogeogro- 
phy  of  the  Monterey  Boy  oreo,  California,  In  Armentrout,  J., 
Cole,  M.R.,  ond  Terbest,  H.,  editors,  Cenozoic  poleogeogro- 
phy  of  the  western  United  States,  Pacific  Section  Society  of 
Economic  Paleontologists  ond  Mineralogists,  Pacific  Coost 
Poleogeogrophy  Symposium  3,  p.  277-296. 

B. —  Hoskins,  E.G.,  and  Griffiths,  J.R.,  1971,  Hydrocorbon  potential 
of  northern  and  central  Colifornio  offshore;  Future  petroleum 
provinces  of  the  United  Stotes — their  geology  and  potentiol: 
Americon  Association  of  Petroleum  Geologists  Memoir  15,  p. 
212-228. 

C—  Howell,  D.G.,  McCulloch,  D.S.,  and  Vedder,  J.G.,  1978,  Gen- 
eral geology,  petroleum  opproisol,  ond  nature  of  environmen- 
tal hazards,  eostern  Pacific  shelf  latitude  28  degrees  to  38 
degrees  north:  U.S.  Geological  Survey  Circulor  786,  29  p. 

D.—  McCulloch,  D.S.,  Clorke,  S.H.,  Jr.,  Dolton,  G.L.,  Field,  M.E., 
Scott,  E.W.,  ond  Utter,  P. A.,  1982,  Geology,  environmentol 
hozords  ond  petroleum  resources  for  1982  OCS  lease  sole  73, 
offshore  centrol  and  northern  Colifornio:  U.S.  Geological  Sur- 
vey Open-File  Report  82-1000,  77  p. 

E. —  McCulloch,  D.S.,  Utter,  PA.,  and  Menock,  J.,  1985,  Mops 
showing  location  of  selected  pre-Quaternory  rock  somples 
from  34°30"  N  latitude  to  42°  N  lotitude,  Colifornio  continen- 
tal margin:  U.S.  Geological  Survey  Miscellaneous  Field  Inves- 
tigation Mop,  MF  1719   (in  press). 

F. —  Vedder,  J.G.,  Beyer,  L.A.,  Junger,  A.,  Moore,  C.W.,  Roberts, 
A.E.,  Toylor,  J.C,  ond  Wogner,  H.C.,  1974,  Preliminory  report 
on  the  geology  of  the  continentol  borderland  of  southern 
California:  U.S.  Geologicol  Survey  Miscellaneous  Field  Stud- 
ies Mop  FM-624,  34  p.,  9  sheets,  scale  1:500,000. 

G.—  Vedder,  J.G.,  Greene,  H.G.,  Scott,  E.W.,  and  Taylor,  J.C, 
1976,  A  summory  report  of  the  regional  geology,  petroleum 
potential,  environmental  geology  ond  technology  for  exploro- 
tion  and  development  in  the  area  of  proposed  lease  sole  48, 
California  continental  borderlond:  U.S.  Geological  Survey 
Open-File  Report  76-787. 

H. —  Vedder,  J.G.,  Crouch,  J.K.,  Scott,  E.W.,  Greene,  H.G.,  Cromer, 
D.,  Ibrahim,  M.,  Tudor,  D.,  and  Vinning,  G.,  1980,  A  summary 
report  of  the  regional  geology,  petroleum  potential,  environ- 
mentol geology,  and  operotionol  considerations  in  the  oreo 
of  proposed  leose  No.  68,  offshore  southern  Colifornio:  US 
Geological  Survey  Open-File  Report  80- 198,  62  p. 

I. — Clorke,  S.H.,  1987,  Geology  of  the  Colifornio  continentol  morgin 
north  of  Cope  Mendocino,  in  Scholl,  D.W.,  Grontz.  A,,  and 
Vedder,  J  G.,  editors.  Geology  and  resource  potential  of  the 
continentol  morgin  of  western  North  America  and  adjocent 
oceon  basins — Beaufort  Seo  to  Boja  California:  Circum  Pa- 
cific Council  for  Energy  and  Mineral  Resources,  Earth  Science 
Series   (in  press) . 


56 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


124° 

120° 

116° 

1 

1 

1 

5 

~  — 1 

;.''-     ( 

1 

'  .  -  ■>         A 

1 

:\   i  ) 

1 

i 

1 

1 

rf:( 

o 

1 

1 
1 

^\  >   2 

^ 

1 

,          100                           0 

100                       ZOOMiles 

1                              100                0 

100             200  Kilometers 

r 

1                        ei5!sa5^5 

^^                 SUBMARINE    CONTOURS   IN    METERS 

\^'.3    I 

/"^-^ 

\ 

'^"..    \. 

Ic^ 

^ 

J 

/    >    1 

^ 

.^ 

^                                                                               \. 

o 

s 

V 

o 

\  ^  1  \ 

♦ 

\ 

^       '?' 

\           ^ 

riS 

:•■  \ 

•n                  / 

^ 

\ 

A                V 

O 

/                 _ 
/ 

^, 

>    o       11               13      V 

\ 

o 
o 

) 

1 

-/- 

W   O*  ''          '='^"-"j    \»30     * 

Vm  e  '^  J^c~~-o~ 

^1 

\  >             )^/-^ 

Figure  3.  Location  map  for  siratigraphic  section}. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


57 


AGE 


^  (D 


1.  Eel  River  Basin 


>- 

■«>f><»io 

) 

cc 

9 

^ 

/ 

< 

C              1 

z 

o    £     o 

iiT  TV 

111 

►- 

5    "     ° 

-I'.— r—    rA 

< 

3 

£         ^ 

o 

"•-^r-^i 

O 

in 

ji  -l,w 

« 

CO 

"• *■  - 

c 

9> 

zr^^ii 

1...  -  iJ 

**■ 

r\-:  -^  A 

O 

---y^^-J 

> 

O 

o 

- 

<r 

o 



< 

i 

— ■ — ^ 

\ 

(E 

*r — ' — 

\ 

UJ 

[to 

"a 

\ 

c 

\l^ 

^^ 

\ 

o 

\ 

""  "^C^ 

o 

UJ 

\ 

-    v^  - 

?\ 

^^ 

Paleo. 

\ 

=^:^- 

CRETACEOUS 

•^^> 

MIDDLE 

? 

:oicM 

JURASSIC 

o--^-o\ 

unconlormlty 

Wildcat  Group 

of 

Ogle  (1953) 

uncon(ormlty 

Bear  River  beds' 

unconlormlty 

Yager 
vterrane  v 


.Coastal 
belt 


te 


oastal- 
rrane 


i-=i)>  faults 


Central 
belt 


■T'ifij^—  unconformity 


2.  Point  Arena  Basin 


basin  edge 
unconformity 


unconformity 


unconformity 
unconformity 


58 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


3.  Bodega  Basin 


basin  edge 
unconformity 


^BS-^^T^^ basin  edge 
".""^^^iv/"  unconformity 


I — unconformity 


unconformity 


AGE 


C   i- 
^  <D 


QUAT 


Holo.  and 
Pleisl. 


< 

QC 
111 


a> 

c 

(D 
O 
O 


Lwr 


Olig. 


CRETACEOUS 


200 


Sandstone 
unconformity 

Clay, silt 

Claystone  and 
siltstone 
Sandstone 
unconformity 

Cherty  shale 


Sandstone 
unconformity 
Shale  with 
volcanic  interbeds 
■  unconformity 
Sandstone 
unconformity 
Brecciated 
sandstone 


4.  Outer  Santa  Cruz  Basin 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


59 


5.  Northern  Monterey  Bay 
Region 


Surficiai  deposits 

Aromas  Sand 
Oeltaic  material 

Purisima  Fm. 

unconformity 

Santa  Cruz  Mudstone 

Santa  Margarita  (?)  Sandstone 
unconformity 

Monterey  Fm. 
unconformity 

Granitic  Basement 


AGE 


1- 
< 

3 

o 

Holocene 

o 
n 

--^--^-_r 

Pleist. 

o 
o 

2K) 

',^;//». 

— -Q p. 1 

> 

< 
1- 

tr 

UI 

Pliocene 

-i-A^ 

e 
c 
« 
o 
o 

i 

o 

3 

MESOZOIC 
OR  OLDER 

X    1    1    1    1 

I  1  1  1  1  1 
■  ■III 

Surficiai  deposits 

Oeltaic  deposits 
Aromas  Sand 
Paso  Robles  Fm. 
Punsima  Fm. 
unconformity 

Monterey  Frn. 

unconformity 
Granitic  Basement 


6.  Southern  Monterey  Bay  Region 


60 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


AGE 


in 

V)  

9   ID 

£5 


7.  Offshore  Santa  Maria  Basin 


QUAT. 

Hoto.  and 
Pleist. 

CO 
CO 

-fc_i   ■■  -  T  Z-^ 

> 
< 
a: 

UJ 

1- 

Pliocene 

in 

B5. 

(0 

c 
« 
o 
o 

5 

d. 

in 

CO 

la 

3^_i^ 

■6 

5 

CO 
in 

CO 

^-f' ^■- 

195 

Olig.  (?) 

219 

eS?x^ 

CRETACEOUS 

? 

yv>'S^ 

and 
JURASSIC 

7 

Oceano  Well 


Foxen  Mudstone 


Sisquoc  Fm. 

Monterey  Fm. 

Obispo  Fm. 
■'■    Lospe  Fm. 

Great  Valley  sequence 

Coast  Range  ophiolite 
Franciscan  Complex 


AGE 


« 

<»_ 

®  in 

c  >- 

y® 

£5 


QUAT 

Hoto  and 
Pteist. 

o 
o 
m 

V  V  v*v  ytf 

> 

< 

1- 
cc 

Ul 

Pliocene 

550 

-^=J 

« 

c 
a> 
u 
o 

o 
o 
n 

BHl^ 

^ 

T^'tF^ 

CRET.  and  JUR. 

250 

^"-^=-:r-Y 

8.  Northern  Santa  Barbara  Channel 
(OSC-CAL  78-164  No.  1) 


^^r^  unconformity 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


61 


9.  Santa  Ynez  Unit  and  vicinity 


3^15-^ /» Offshore  subsurface 


Sisquoc  Formation 


Monterey  Formation 

Bentonite 
Rincon  Shale 
Vaqueros  Formation 
Alegrla.Gaviota  and 
Sespe  Formations 

Sacate  Formation 
Cozy  Dell  Shale 
Matilija  Sandstone 

Anita  CI  Shale 

Unconf. 

Jalama  Formation 


)>\N.  Santa  Ynez  Mts. 


-I5^:.^rS       Espada  Formation 


Fault  (?) 
Franciscan  Complex 


AGE 


U 


> 

< 

(C 
UJ 

t- 

« 

c 
e 
o 
o 

OL 

d 

=> 

o 

* 
o 

o 
m 

o 
in 

ff  otSiVo 

( 

'  '  0.  ■  '- 

• 

o 
c 
o 
u 
o 

i 

d 

1/) 
in 

I 

o 

o 

Olig. 

Eocene 

LATE 
CRETACEOUS 

to 

'VN.^^^WN 

Pico" 
Formation 

Repetto" 
Formation 


10.  Dos  Quadras  Oilfield  and  vicinity 


unconformity 

Section  inferred 
below  'Repetto'  Fm. 


62 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


M  — 

Q)  CO 

c  ^ 

U  (D 


AGE 


11.  San  Miguel  Island 


£J--sM  -unconformity 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


63 


AGE 


a>  m 

.9fl5 
F2 


12.  Santa  Rosa  Island 


QUATERNARY 

100 

i»»'.«.4 

-  u 

o 
o 

CO 

0-    V-O     6 

^'^Zzl 

•ooooao 

>A 

400 

oeo  ooopp\ 

« 

To  o  o  *  0  o 

^ 

A  »  ■  «■  aajr 

■■ 

•o 

v;;.v.vM 

TJ 

.\ 

? 

;>>iaa  »»  ^a^vl 

*tf eo      ft  « 

<4 

w 

o 

o 

CJ) 

*  ■  T-'-' " " 

" 

r\j 

c 

1^ 

a> 

B    «    0  «  O  O  0\ 

o 

».»"«%Jr  «'^"* 

■  iC 

o 

"*»•»•"•■ 

» 

^ 

■  Ba«B^'';(«ri^ 

. 

V 

r'^_r"=.~. 

^_  _| 

>- 

cc 

o 

3^3^3 

< 

i_ 

o 

— — 

cc 

S 

CM 

^zr^zETi 

o 

_  _    , 

LU 

_i 

— 

1- 

_^~    -~^. 

_-!_'_ 

0    0     o 

0     o"o    tt 

-TT    5~B  a 

o 

i  O  OOOo 

in 

c^a  ooo< 

Oligocene 

0  o  o  a  oc 

^~ 

0  O  0O  004 
4  0  ©•Otf 

i 

-—■- 

(D 

tr-'^V 

<D 

o 

u 

o 

•.-■'•fc 

o 

o 

-i-^'M 

111 

•» 

^-L 

i^  i^-^^ 

nconformity 


Fault 


64 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


AGE 


13.  Santa  Cruz  Island 


QUAT. 


>- 

IT 

< 


Pliocene  85/ 


Oligo- 
cene 


100 


B   O    O  0-0 

■rrr 


»e«  o  oo  0  4 


=  unconformity 


ii».Jr—  ""conformity 


»0OOOOOO 


Bod  AO  90 


tf ••oe«04 


es«B  •»••« 

•.V.'.V.'. 

O  ••  b  O  *« 

a  g  ft  a  ■  tj 


9       Red 
beds 


seclion  unknown 


I  subsurface  only 


< 
I- 

cc 

Ul 


o 

c 

u 
o 

UJ 


Paleo- 
cene 


OOO  00«04 


•-<T  -»T> 


w 

o 

Ul 

o 

< 
t- 

UJ 
CE 


Sfclton  uf? 


known 


3 
,_     O 

a  o 
a.  n 

o 


'»  e  •  ei   b  o  I 
)   »  6  •  o  A  J 

'  ■  *!  7 


kCSO. 

Pre.  U. 
Crtl. 

^^4^ 

.  subsurface  only 


Fault 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


65 


AGE 


14.  Northeast  Coast  Santa  Cruz 
Island 


> 
a: 
< 
t- 
cc 

Hi 

*- 

Holo  and  / 

Mio     Iji 

cene    tin 

J^ 

Ke^ 

o 

*     >     V    «'    <  V 

k    V     ><     A     J      < 

400 

189 

Ag. 
und«t«rmin«d 

o 
o 

^:^ 

MESOZOIC 

7 

Monterey  Formation 

Santa  Cruz  Island    Volcanic* 
of  NoK  and  Nolt  (19691 

■  3  San  Onoira  Breccia 


Franciscan  Complex 


Lllhol  ogles 
Inferred  In  part 


AGE 

CO  » 

3)  V 

Qual. 

Holo  and 
Pleistocene 

o 

o 
en 

^'Jr-'J 

'Pico'  Formation 

> 

< 

IT 
UJ 

V- 

• 
% 

d 

3 

O 

o 

=:"=^~ 

-J 

o 
1/) 

'-=-1Mj 

'Repatto'  Forma 

• 
c 
• 

■o 
c 
■ 

2 

o 
in 

\ 

Monterey  Stiale 

? 

7 

unconformity 

MESOZOIC 

;;';?53] 

Catalina  Shale 

1 

inf 

.itriot  ogles 
erred  in  part 

15.  Offshore  Santa  Monica  Basin 


66 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


AGE 


M 

C    •- 

£5 


16.  Northern  Santa  Rosa-Cortes  Ridge 


QUAT.Holo./Plast. 

170 

—^    -Zi 

>- 

DC 

< 

tr 

UJ 

1- 

Miocene 

O 

in 
o 

=  '=-j:—. 

Olig. 

o 

^0  0  0 

Eocene 

o 

CO 

■—.  —   — 

Paleo. 

o 

in 

'qO  o~o  o     ^ 

o 

111 
o 
< 

(- 

LU 
CC 

o 

0) 
Q. 

a 

3 

o 

CO 

o 

=-—  -J 

-7  —  •?- 

o 
o 

3 
3 


AGE 


_^    <D 

£2 


17.  Northern  Patton  Ridge 


unconformity 

r^j--^- Fault? 

-p^i /'  \  Espada  (?)  Fm. 

yy^r  /  ^  I    Mesozoic  ? 

Franciscan  (?) 
Complex 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


67 


AGE 


22 

n 


18.  Santa  Cruz-Catalina  Ridge 


Quat. 

Holo./Pleisl 

60 

^::;.^-virrTi 

1- 

Pliocene 

iiin 

■  ■  -.■.•-■"7 

6 

3 

2 

o 

>-*v*^^T4) 

MESOZOIC(?) 

? 

a'M 

Older  strata  (?) 
Catalina  Schist 


Thicknesses 
inferred  in  part 


AGE 


c  is 


Ouat. 

Nolo  /Pleisl 

o 

— .■   — ■ 

> 
tr 
< 

1- 

1- 

c 

o 

g 

d. 

=3 

o 

(O 
CO 

^  ""— 

(D 

$ 
O 

_l 

o 
o 

CM 

T-^-r" 

e 

c 

0) 

o 
o 

2 

Q. 

1 

■6 

5 

o 
o 

00 

? 

///// 

MESOZOIC 

? 

■Pico'  Fornnation 


■Repetto'  Formation 
(central) 


Monterey  Shale 
(north  edge) 

Catalina  Schist 


19.  San  Pedro  Basin 


Lithologies 
inferred  in  part 


68 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


AGE 


P  5 


20.  Newport  Beach- 
Dana  Point  Shelf 


unconformity 
Nigel     Fornnation 

Caplstrano  Formation 
Monterey  Shale 

San  Onofre  Breccia 
Topanga  Formation 

Vaqueros  Formation 

Sespe  Formation  (nonmarine) 

Santiago  Formation 
Fault(?) 
Silverado  Formation 


^~— ~— V     Williams  Formation 

- —  -  -\\    FaultC)  Ladd  Formation 

'  'nconformity 

Santiago  Peak  Volcanics 


unconformity 
igc 

Bedford  Canyon  Formation 


AGE 


C     •- 


QUATERNARY 

7 

».a«aQo 

> 
tr. 

< 

LU 

9) 
C 
Q> 
U 

o 

100, 

o 

o 

(D 

■  ■■*•■' 

? 

^'-  '■-  *■/ 

MESO. 

Pre-U. 
Cret. 

7 

m 

—  unconformity 


Fault 


21.  Santa  Catalina  Island 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


69 


AGE 


22.  San  Nicolas  Island 


QUAT. 


>- 

tr 

a> 

< 

c 

cr 

o 

Ol 

Ol 

0-' 


i^"n- 


jTa  S^^ 


--  unconformity 


AGE 


(0 

in  — 
j:5 


UJ 

1- 

Mio. 

o 

i 

o 

CO 

=  -3-^ 

'^  y    <  -f  r 

^   <      V    A 

MESOZOIC(?) 

7 

/,    /    //// 

23.  San  Clemente  Ridge 


unconformity 


AGE 


in  ^ 

O    (A 

5  5 


24.  Southern  Guff  of  Santa  Catalina 


QUAT 

Nolo   'Pt.tll 

150 

j.>  C^__>J 

> 

< 
t- 

a 

Plioc»n« 

a 

O 

5r>>1-( 

d 

2 

2 

3 

o 

o 
o 

*  »   <       V 

MESOZOfCI?) 

7 

i:.'i<1 

unconformity  (?) 
Older  strata  (?) 
Cataima  Sctiist 


Littioiogies  and  thicknesses 
Interred  In  part 


70 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


AGE 


^5 


25.  San  Clemente  Island 


Ouat. 

Pliocene 

100 

•■     \ 

> 

< 

1- 
CC 
LU 

1- 

IS 

c 

<B 
O 
O 

i 

0) 

■o 

300 

o 
o 
in 

unconformity 
unconformity 


AGE 


vt 

{/)  ^ 
■D  (B  „ 
<D  c    i- 

c£5 


QUAT. 
-•?-■?- 

Holocene  to 

o 
o 

9 

Pliocene 

CO 

-i 

o 

MiO. 

o 

o 

? 

> 

< 

1- 

Oligocene 

UJ 

and  (or) 

o 

1- 

Eocene 

■<f 

9 

and  (or) 

Paleocene(? 

7         f 

CRETA- 

o 

o 

9 

CEOUS 

a 

in 

o 

26.  San  Nicolas  Basin 


AG 


lE  (5  2 


27.  Dall  Bank 


1- 

UJ 

(- 

Miocene 

o 

rs. 
r) 

J;/j^ 

Oligocene 

60 

Eocene 

o 

00 

CRETA- 

a. 
a. 

o 

CEOUS 

3 

L. 

o 
at 
n 

— 

1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


71 


28.  Thirtymile  Bank 


AGE 


So 


QUAT 

Holo./Pleisl. 

SO 

=L  .  ■^_  .  - 

CC 
liJ 

Pliocene 

120 

^^__— _r- 

MiO. 

■D  d 

o 
o 
o 

MESOZOIC  (?) 

(?) 

^;;a24 

Catalina  Schist 


Lithologies  and  thicknesses 
Inferred  In  part 


AGE 

"3 
^1 

OUAT 

Holo.'Pleisl. 

120 

-.--.--{ 

> 

a: 

< 
1- 

Hi 

1- 

Pliocene 

340 

;^-__.  ^^ 

d 

T3 

C      . 

s 

o 
in 

Eocene 

280 

-^—s.-'X 

CRETA- 
CEOii'5 

Q. 
Q. 
3 

o 
to 

K-f-y/il 

JURA 

SSIC 

2 
d 

3 

7 

A      7"J       A 

San  Diego  Formation 

(Coronado  Bank) 
Unconf.(?l  Monterey  Shale 
Unconf.       "-a  Jolla  Group 
Cabrillo  Formation 
Pt.  Loma  Formation 
Unconf.     Lusardi  Formation 
S.  C.  batholith 

Santiago  Peak  Volcanics 


29.  San  Diego  Shelf 


30.  Fortymile  Bank 


AGE 

o  in 

i5? 

PUAr 

E 
UJ 

»- 

Molo  to  Pllo 

100 

^~='\ 

MiO. 

o 

o 
o 
o 

M% 

1 

MESOZOIC  C) 

7 

g£2g 

L 
lnt< 

ithoiogies 
»rred  in  part 

Unconformity 
Catalina  Schist 


72 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


AGE 


.^2 


31.  Central  Blake  Knolls 


TERT. 

Miocene 

370 

:>iX.\ 

MESOZOC  (?) 

? 

////// 

unconformity 
Catalina  Schist 


AGE 


O  (0 


cc 

< 
1- 

UJ 

Mio. 

L. 
anC 

M. 

o 
o 

?--l(^ 

^    V    <     V    Aj 

Oligocene 

U 
o 

^^-=_| 

Eocene 

o 
<o 
in 

uS^ 

Paleocene 

270 

^_  ■_:  _ 

CRETA- 
CEOUS 

« 
a 
a 

D 
"O 

c 
a 

e 

o 

o 
o 

_7 7- 

\ 

32.  Cortes  Bank 
(OSC-CAL  75-70  No.   1) 


unconformity 


TD  3100  m 


33.  Northeast  Bank 


AGE 


CO  . 
0)    0) 

C   != 


P'S 


cc 

UJ 

Pllocene 
—  7  — ?- 

Miocene 

o 
m 

00 

A      <     1   »' 

r  -r  V   > 
-I    <  7^1' 

1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


73 


BIBLIOGRAPHY 


This  bibliography  includes  those  references  studied  and, 
in  part,  used  to  compile  the  California  continental  margin 
geologic  maps.  Also  included  are  references  that,  because 
of  their  scale  or  subject,  were  not  used  directly  in  this 
compilation,  but  which  may  be  useful  to  investigators  in- 


volved in  geologic  studies  within  the  region.  The  refer- 
ences consist  of  published  geologic  data  and  unpublished 
Master's  and  Doctoral  theses  that  are  readily  available,  as 
well  as  open-file  reports,  administrative  reports  and  re- 
cently released  proprietary  data. 


AqIIo,  K.R.,  1982,  The  Franciscan  Complex  of  northernmost  Califor- 
nia: sedimentation  and  tectonics,  in  leggett,  J.K.,  editor.  Trench 
forearc  geology,  sedimentation  and  tectonics  on  modern  and 
ancient  active  plate  margins:  Geological  Society  of  London,  p. 
419-432. 

Adoms,  M.V.,  1973,  Report  on  water  injectivity  test,  lease  OCS-P 
0241,  well  number  B-49-1,  Dos  Cuadros  Field,  Santa  Barbara 
Channel,  off  California:  U.S.  Geological  Survey  Circular  687,  28 

P 

Agnew,  D.C.,  1979,  Tsunami  history  of  San  Diego,  in  Abbott,  P.L. 
and  Elliott,  W.J.,  editors.  Earthquakes  and  other  perils,  San 
Diego  region:  San  Diego  Association  of  Geologists  Guidebook, 
p.  117122. 

Agnew,  D.C.,  Legg,  M.,  and  Sirond,  C,  1979,  Earthquake  history  of 
San  Diego,  in  Abbott,  P.L.  and  Elliott,  W.J.,  editors.  Earthquakes 
and  other  perils,  San  Diego  region:  Son  Diego  Association  of 
Geologists  Guidebook,  p.   123-138. 

Albee,  A.L.,  and  Smith,  J.L.,  1966,  Earthquake  characteristics  and 
fault  activity  in  southern  California,  in  Lung,  R.,  and  Proctor,  R., 
editors.  Engineering  geology  in  southern  California:  Association 
of  Engineering  Geologists  Special  Publication,  p.  9-33. 

Aldrich,  J.K.,  1969,  Grovity  of  northern  Channel  Islands:  American 
Association  of  Petroleum  Geologists  Bulletin,  v.  53,  p.  470. 

Aldrich,  J.K.,  1969,  Grovity  survey  of  the  Santo  Barbara  Channel 
Islands:  University  of  California,  Sonto  Barbara  unpublished 
Master's  Thesis. 

Allen,  A. A.,  and  Schleuter,  R.S.,  1969,  Estimates  of  surface  pollution 
resulting  from  submorine  oil  seeps  ot  Cool  Oil  Point  ond  Platform 
A:  General  Research  Corporation,  Santo  Barbara,  California, 
Technical  Memorandum  1230,  43  p. 

Allen,  A. A.,  Schleuter,  R.S.,  and  Mikolaj,  P.G.,  1970,  Natural  oil 
seepage  at  Coal  Oil  Point,  Santa  Barbara,  California:  Science, 
V.  170,  p.  974-977. 

Allen,  C.R.,  St.  Amond,  P.,  Richter,  C.F.,  ond  Nordquist,  J.M.,  1965, 
Relationship  between  seismicity  and  geologic  structure  in  the 
southern  California  region:  Seismological  Society  of  America 
Bulletin,  V.  55,  p.  753-797. 

Allen,  C.R.,  Silver,  L.T.,  and  Stehli,  F.G.,  1960,  Aguo  Blanco  fault — a 
major  transverse  structure  of  northern  Bajo  California,  Mexico: 
Geological  Society  of  America  Bulletin,  v.  71,  p.  457-482. 

Allen,  D.R.,  and  JoujonRoche,  J.E.,  1958,  West  Newport  Oil  Field: 
American  Association  of  Petroleum  Geologists  and  Society  of 
Economic  Paleontologists  and  Mineralogists,  Pacific  Section, 
Guidebook,  p.   142- 144. 

Alpha,  T.R.,  1970,  Physiographic  diagrams  of  ports  of  the  continen- 
tal borderlands  of  California  and  Alosko:  U.S.  Geological  Survey 
Open  File  Report  70-5. 

Alpha,  T.R.,  1971,  Physiographic  diagram  of  southern  California,  in 
Elders,  W.A.,  editor.  Geological  excursions  in  southern  Califor 
nio:  Geological  Society  of  America,  Cordilleran  Section  Meeting, 
University  of  California,  Riverside. 

Alpha,  T.R.,  1972,  Physiographic  diagrams  for  Venturo-Oxnard  off- 
shore, Astoria  Canyon  and  Fon,  Newport,  Northern  Bering  Seo, 
the  Aleutian-Kamchotko  convergence,  Caribbeon  Arc-Hitpaniolo 


to  Guadalupe,  Bohio  de  Compeche,  British  Honduras  and  Vene- 
zuelan borderlond:  U.S.  Geological  Survey  Open  File  Report 
72-5,  9  sheets. 

Alpha,  T.R.,  1978,  Oblique  mop  of  Monterey  Boy,  California:  U.S. 
Geological  Survey  Open-File  Report  78-681. 

Alpha,  T.R.,  1978,  Southern  California  borderland;  oblique  map  of 
the  northwestern  part:  U.S.  Geological  Survey  Open-File  Report 
78-967. 

Alpha,  T.R.,  1978,  Regional  geologic  and  geophysical  base  mops  of 
western  North  America  and  adjacent  oceans:  U.S.  Geological 
Survey  Open-File  Report  78-603. 

Alpha,  T.R.,  1980,  Oblique  map  of  the  Pacific  Coast  of  North  Ameri- 
co,  U.S.  Geological  Survey  Open-File  Report  80-93. 

Alpha,  T.R.,  and  Gerin,  M.,  1980,  Oblique  mop  of  the  northern 
California  continental  margin:  U.S.  Geological  Survey  Open-File 
Report  80-195. 

Alpho,  T.R.,  Dingier,  J.R.,  Jones,  D.R.,  Molion,  D.E.,  Peterson,  DC, 
and  Morely,  J.M.,  1981,  Physiographic  diagram  of  the  upper 
Cormel  Canyon  and  Point  Lobos,  California:  U.S.  Geological 
Survey  Open-File  Report  81-440. 

Anderholt,  R.,  LeFever,  R.D.,  and  Reed,  W.E.,  1977,  Texture  versus 
depth,  and  mainland  versus  offshore  relationships,  southern  Cali- 
fornia borderland:  Geological  Society  of  America  Abstracts  with 
Programs,  v.  9,  p.  379. 

Anderholt,  R.,  and  Reed,  W.E.,  1978,  Organic  corbon  and  texture 
of  benthic  and  intertidol  sediments,  southern  California  continen- 
tal borderland:  Geologicol  Society  of  America  Abstracts  with 
Programs,  v.  10,  p.  358. 

Anderson,  D.L.,  1971,  The  Son  Andreas  fault:  Scientific  Americon, 
v.  255,  p.  53-66. 

Anderson,  J.G.,  1979,  Estimating  the  seismicity  from  geologic  struc- 
ture for  seismic  risk  studies:  Seismological  Society  of  America 
Bulletin,  V.  69,  p.  135  158. 

Anderson,  J.G.,  1984,  The  September  4,  1981  Sonto  Borboro  Islond, 
California  earthquake:  Interpretation  of  strong  motion  doto:  Bul- 
letin of  the  Seismological  Society  of  America,  v.  74,  p,  995-1010. 

Anderson,  J.G  ,  Trifunoc,  M.D.,  Teng,  T.L.,  Amini,  A.,  and  Moslem, 
K.,  1981,  Los  Angeles  vicinity  accelerogroph  network:  University 
of  Southern  Californio,  Department  of  Civil  Engineering  Report 
CE  81-04 

Anderson,  RE.,  Redwine,  I.E.,  and  McGovney,  P.E.,  1949,  Geology 
of  northern  Sonto  Rosa  Island,  California:  American  Associotion 
of  Petroleum  Geologists  Bulletin,  ».  33,  p.  2062. 

Andrews,  R.S.,  Cepk,  R.J.,  and  Wilson,  O.B.,  Jr.,  1972,  Moss  physi- 
cal and  acoustic  properties  of  sediments  from  the  Monterey 
Submarine  Fan:  American  Geophysicol  Union  Transactions,  v. 
53,  p.  1028. 

Arends,  R.G.,  1980,  Diatoms  and  silicoflogellates  from  Molocene 
sediments,  southern  California  continental  borderland;  American 
Association  of  Petroleum  Geologists  Bulletin,  v.  64,  p.  438. 

Arleth.  K.F.,  1977,  Marine  structural  geology  and  geologic  evolution 
south  of  Santo  Rosa  and  Son  Miguel  Islands,  California:  San 
Diego  Stote  University  unpublished  Mosler's  Thesis. 


74 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


Arleth,  K.F.,  1979,  Structure  ond  seismic  stratigraphy  south  of  Santa 
Rose  and  San  Miguel  Islands,  California:  Geological  Society  of 
America  Abstrocts  with  Programs,  v.   11,  p.  380. 

Arnol,  R.E.,  1976,  Miocene  poleobathymetric  chonges  of  the  Sonto 
Rosa-Cortes  Ridge  area,  Colifornia  continental  borderland,  in 
Howell,  D.G.,  editor.  Aspects  of  the  geologic  history  of  the 
Colifornio  continental  borderland:  American  Associotion  of  Pe- 
troleum Geologists,  Pacific  Section,  Miscellaneous  Publicotion 
24,  p.  60-79. 

Arnol,  R.E.,  1980,  Comparison  of  Miocene  provincial  forominlferol 
stages  to  Coccolith  zones  in  the  California  continental  border- 
land. Comment:  Geology,  v.  8,  p.  2-4. 

Arnol,  R.E.,  and  Vedder,  J.G.,  1976,  Changes  in  Miocene  poleoboth- 
ymetry  of  the  California  continental  borderland  north  of  32  de- 
grees: American  Association  of  Petroleum  Geologists  Bulletin,  v. 
60,  p.  646. 

Arnal,  R.E.,  and  Vedder,  J.G.,  1976,  Late  Miocene  poleobothymetry 
of  California  continental  borderland  north  of  32  degrees:  Ameri- 
can Association  of  Petroleum  Geologists  Bulletin,  v.  60,  p.  2174. 

Arnol,  R.E.,  ond  Vedder,  J.G.,  1976,  Late  Miocene  poleobothymetry 
of  the  California  continental  borderland  north  of  32  degrees,  in 
Fritche  and  others,  editors,  The  Neogene  symposium:  Society  of 
Economic  Paleontologists  and  Mineralogists,  Pacific  Section,  San 
Francisco,  p.  1-8. 

Ashley,  R.J.,  1974,  Offshore  geology  and  sediment  distribution  of 
the  El  Capiton  -  Govioto  continental  shelf,  north  Santo  Barbara 
Channel,  California:  Son  Diego  State  University  unpublished 
Master's  Thesis. 

Ashley,  R.J.,  Berry,  R.W.,  and  Fischer,  P. J.,  1977,  Offshore  geology 
ond  sediment  distribution  of  the  El  Copiton  -  Gaviota  continental 
shelf,  northern  Sonto  Barboro  Channel,  California:  Journol  of 
Sedimentory  Petrology,  v.  47,  p.  199-208. 

Atwoter,  B.F.,  1978,  Centrol  Son  Mateo  County,  Californio:  Lond- 
use  controls  arising  from  erosion  of  seacliff,  londsliding,  and  fault 
movement:  U.S.  Geological  Survey  Professional  Paper  950,  p. 
11-19. 

Atwoter,  B.F.,  Foss,  B.E.,  and  Wehmiller,  J.F.,  1981,  Stratigraphy  of 
Lote  Quaternary  estuorine  deposits  and  amino  ocid  stereochem- 
istry of  oyster  shells  beneath  Son  Francisco  Bay,  California:  Quo- 
ternary  Research,  v.  16,  p.  181-200. 

Atwoter,  B.F.,  Hedel,  C.W„  ond  Helley,  E.J.,  1977,  Late  Quaternary 
depositionol  history,  Holocene  seolevel  changes  and  vertical 
crustol  movement,  southern  Son  Froncisco,  Boy,  California:  U.S. 
Geological  Survey  Professional  Paper  1014,  p.  15. 

Atwoter,  T.,  1970,  Implications  of  plote  tectonics  for  the  Cenozoic 
tectonic  evolution  of  western  North  America:  Geologicol  Society 
of  America  Bulletin,  v.  81,  p.  3513-3536. 

Atwoter,  T.,  1972,  A  detailed  near-bottom  geophysical  study  of  the 
Gordo  Rise  ond  implications  of  plate  tectonics  for  the  Cenozoic 
tectonic  evolution  of  western  North  America:  University  of  Coli- 
fornia, Son  Diego,  unpublished  Doctoral  Thesis. 

Atwoter,  T.,  and  Molnor,  P.,  1973,  Relotive  motion  of  the  Poclfic  ond 
North  Americon  plates  deduced  from  seafloor  spreading  In  the 
Atlantic,  Indian,  and  South  Pacific  Oceons,  in  Kovoch,  R.L.,  ond 
Nor,  A.,  editors,  Proceedings  of  the  conference  on  tectonic  prob- 
lems of  the  San  Andreas  fault  system:  Stanford  University  Publi- 
cations in  Geological  Science,  v.   13,  p.  136-148. 

Atwoter,  T.M.,  ond  Mudie,  J.D.,  1968,  Block  faulting  on  the  Gordo 
Rise:  Science,  v.   159,  p.  729  731. 

Auld,  B.,  Latham,  G.,  Nowroozi,  A.,  and  Seeber,  L.,  1969,  Seismo- 
loglcol  evidence  of  the  tectonics  of  central  and  northern  Califor 
nio  determined  from  oceon  bottom  seismic  meosurements: 
Seitmological  Society  of  America  Bulletin,  v.  59,  p.  2001-2015. 


Austin,  C.F.,  1968,  Geologic  evoluation  of  Son  Clemente  Island  as 
o  locotion  for  o  rock-site  1  instollotion:  Naval  Weopons  Center 
Technlcol  Publication,  NWC  TP4501,  24  p. 

Avila,  F.A.,  1968,  Middle  Tertiary  stratigraphy  of  Sonto  Rosa  Island, 
Californio:  University  of  California,  Sonto  Borboro  unpublished 
Moster's  Thesis. 

Avilo,  F.A.,  and  Weaver,  D.W.,  1969,  Mid-Tertiary  strotigrophy, 
Santa  Rosa  Islond,  in  Weaver,  D.W.,  and  others,  editors.  Geol- 
ogy of  the  northern  Channel  Islands:  American  Association  of 
Petroleum  Geologists  and  Society  of  Economic  Paleontologists 
and  MInerologlsts,  Poclfic  Section,  Speciol  Publicotion,  p.  48-67. 

Aydin,  A.,  Poge,  B.M.,  1984,  Diverse  Pliocene-Quoternory  tectonics 
in  o  transform  environment.  Son  Francisco  Boy  region,  Colifornio: 
Geological  Society  of  America  Bulletin,  v.  95,  p.  1303-1317. 

Azmon,  E.,  1960,  Heavy  minerals  in  sediments  of  southern  Colifor- 
nio: University  of  Southern  Californio  unpublished  Doctoral  The- 
sis. 

Boche,  A.D.,  1855,  Notice  of  eorthquoke  woves  on  the  western  coast 
of  the  United  States,  on  the  23rd  ond  25th  December,  1854:  U.S. 
Coast  Survey  Annual  Report,  p.  342-346. 

Bochmon,  SB.,  1978,  A  Cretaceous  and  early  Tertiary  subduction 
complex,  Mendocino  coast,  northern  Colifornio,  in  Howell,  D.G. 
and  McDougoll,  K.A.,  editors,  Mesozoid  poleogeogrophy  of  the 
western  United  States:  Pacific  Coast  Poleogeogrophy  Sympo- 
sium 2,  Society  of  Economic  Poleontologists  ond  Mineralogists, 
Pacific  Section,  Los  Angeles,  p.  419-430. 

Bochmon,  S.B.,  1979,  Sedimentation  and  morgin  tectonics  of  the 
coostol  belt  Franciscan,  Mendocino  coost,  northern  Colifornio: 
University  of  California,  Davis,  unpublished  Doctoral  Thesis. 

Bochmon,  S.B.,  1982,  The  Coostol  belt  of  the  Fronciscon — younger 
phose  of  northern  California  subductions,  in  Leggett,  J.K.,  editor, 
Trench-foreorc  geology:  sedimentation  and  tectonics  on  modem 
and  ancient  active  plate  margins:  Geological  Society  of  London, 
p.  401-418. 

Bochmon,  S.B.,  Underwood,  M.B.,  ond  Menock,  J.S.,  1984,  Cenozoic 
evolution  of  coostol  northern  Californio,  in  Crouch,  J.K.,  ond 
Bochmon,  S.B.,  Tectonics  ond  sedimentolon  along  the  Californio 
margin:  Society  of  Economic  Paleontologists  ond  MInerologlsts, 
Pocific  Section,  v.  38,  p.  55-66. 

Bock,  William,  1957,  Geology  and  ground  woter  feotures  of  the 
Smith  River  Ploln,  Del  Norte  County,  Colifornio:  U.S.  Geologicol 
Survey  Water  Supply  Paper  1254,  76  p. 

Boddley,  E.R.,  1954,  Geology  of  the  South  Mountoin  Oil  Field, 
Venturo  County  Mop  Sheet  29,  in  Johns,  R.H.,  editor,  Geology 
of  southern  Colifornio:  Colifornio  Deportment  of  Noturol  Re- 
sources, Division  of  Mines  Bulletin  170. 

Bailey,  E.H.,  1940,  Pledmontlte  ond  kyonite  from  the  Fronciscon  of 

Sonto  Cotolino  Island:  Geological  Society  of  America  Bulletin,  V. 

51,  p.  1955. 
Boiley,  E.H.,    1941,  Minerology,  petrology,  and  geology  of  Sonto 

Cotolino  Island,  Colifornio:  Stonford  University  unpublished  Doc- 

torol  Thesis. 
Boiley,  E.H.,  1954,  Rood  log  for  Santa  Cotalina  Island:  Geological 

Society  of  Americo  field  trip,  mop:  Generalized  geologic  mop  of 

Sonto  Cotolino  Islond,  scale  1:82,000. 

Boiley,  E.H.,  1967,  Rood  log  for  Sonto  Cotolino  Islond,  American 
Association  of  Petroleum  Geologists  field  trip,  April  14-15,  1967: 
Americon  Association  of  Petroleum  Geologists,  Poclfic  Section, 
21  p. 

Bailey.  E.H.,  Irwin,  W.P.,  ond  Jones,  D.L.,  1964,  Fronciscon  ond 
reloted  rocks,  ond  their  signiflconce  in  the  geology  of  western 
California:  California  Division  of  Mines  ond  Geology  Bulletin 
183,  177  p. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


75 


Balozs,  E.I.,  and  Douglas,  B.C.,  1979,  Geodetic  leveling  and  the  sea 
level  slope  along  the  California  coast:  Journal  of  Geophysical 
Reseorch,  v.  84,  p.  6195-6206. 

Bollantyne,  R.S.,  1983,  Estimoted  oil  and  gas  reserves,  southern 
Californio  outer  continental  shelf:  U.S.  Geological  Survey  Open- 
File  Report  83-559. 

Bandy,  O.L.,  1953,  Ecology  and  paleoecoiogy  of  some  California 
foraminifers.  Port  II,  forominiferol  evidence  of  subsidence  rates 
in  the  Ventura  basin:  Journal  of  Paleontology,  v.  27,  p.  200-203. 

Bandy,  O.L.,  1963,  Larger  living  foraminifera  of  the  continental 
borderland  of  southern  Colifornio:  Cushman  Foundation  for 
Forominiferol  Research  Contributions,  v.   14,  p.   121-126. 

Bandy,  O.L.,  Ingle,  J.C,  and  Risig,  J.M.,  1964,  Focies  trends  Son 
Pedro  Bay,  Colifornio:  Geological  Society  of  America  Bulletin,  v. 
75,  p.  403-424. 

Borbot,  W.F.,  1958,  The  Los  Angeles  basin  oreo,  California,  in 
Weeks,  L.G.,  editor.  Habitat  of  oil — a  symposium:  American 
Association  of  Petroleum  Geologists,  p.  62-77. 

Barnes,  B.B.,  1970,  Marine  phosphorite  deposit  delineation  tech- 
niques tested  on  the  Coronodo  Bonk,  southern  California:  Second 
Annual  Offshore  Technology  Conference,  Houston,  Texas,  paper 
number  OTC  1259,  p.  315,  349. 

Barnes,  P.W.,  1969,  Bathymetry  and  sedimentary  structures  of 
Santo  Cruz  bosin,  California:  American  Association  of  Petroleum 
Geologists  Bulletin,  v.  53,  p.  461-462. 

Barnes,  P.W.,  1970,  Marine  geology  and  oceonography  of  Sonto 
Cruz  basin  off  southern  California:  University  of  Southern  Coli- 
fornio, Department  of  Geological  Sciences  Report  USC-GEOL 
70-3,  175  p. 

Bornes,  R.O.,  Bertine,  K.K.,  and  Goldberg,  E.D.,  1975,  N2:Ar,  nitrifi- 
cation and  denitrificotion  in  southern  California  borderland  basin 
sediments:  Limnology  and  Oceanography,  v.  20,  p.  962-970. 

Barrows,  A.G.,  1974,  A  review  of  the  geology  and  earthquake 
history  of  the  Newport-lnglewood  structural  zone,  southern  Cali- 
fornia: California  Division  of  Mines  and  Geology  Special  Report 
114,  155  p. 

Borton,  C.L.,  1976,  Carbonate  surface  sediments  of  Tanner  and 
Cortes  bonks,  California  continentot  borderland:  University  of 
California,  Los  Angeles,  unpublished  Moster's  Thesis. 

Boss,  R.O.,  1960,  Geology  of  the  western  portion  of  the  Point  Dume 
quadrangle,  Los  Angeles  county,  Colifornio:  University  of  Califor- 
nia, Los  Angeles,  unpublished  Master's  Thesis. 

Bauer,  W.E.,  Cohn,  A. A.,  LeConte,  J.,  Pickett,  E.S.,  ond  Truex,  J.N., 
1966,  A  tour  of  the  coastal  oil  fields  of  the  Los  Angeles  basin  and 
adjacent  to  Son  Pedro  Boy,  Colifornio:  American  Association  of 
Petroleum  Geologists,  Society  of  Exploration  Geophysicists,  and 
Society  of  Economic  Paleontologists  and  Mineralogists,  Joint 
Annual  Field  Trip,  Long  Beach,  California,  8  p. 

Beer,  R.M.,  and  Gorsline,  D.S.,  1971,  Distribution,  composition,  and 
transport  of  suspended  sediment  in  Redondo  Submorine  Conyon 
and  vicinity,  California:  Morine  Geology,  v.   10,  p.   153-176. 

Bereskin,  S.R.,  1969,  Miocene  biostrotigrophy  of  southwestern 
Santa  Cruz  Islond,  California:  Americon  Association  of  Petroleum 
Geologists  Bulletin,  v.  53,  p.  469. 

Bereskin,  S.R.,  ond  Edwords,  L.N.,  1969,  Mid-Tertiory  stratigrophy, 
southwestern  Sonto  Crui  Island,  in  Weaver  and  others,  editors. 
Geology  of  the  northern  Channel  Islonds:  Americon  Associotion 
of  Petroleum  Geologists  and  Society  of  Economic  Poleontologists 
ond  Minerologists,  Pocific  Section,  Special  Publication,  p.  68-79. 

Berger,  R,  1966,  Radiocarbon  content  of  marine  shells  from  the 
Colifornio  and  Mexican  west  coast:  Science,  v    153,  p   864  866. 

Berger,  W  H  ,  1969,  Anoerobic  basin  sedimentation  ond  differential 
preservotion  of  plonktonic  foraminifers,  Sonto  Barbara  basin: 
American  Association  of  Petroleum  Geologists  Bulletin,  v.  53,  p. 
468. 


Bergquist,  J.R.,  1978,  Depositionol  history  and  fault-related  studies, 
Bolinos  Lagoon,  California:  U.S.  Geological  Survey  Open-File 
Report  78-802,  p.  164. 

Bernstein,  R.L.,  Breaker,  L.,  and  Whritner,  R.,  1977,  California  current 
eddy  formation:  ship,  air,  and  satellite  results:  Science,  v.  195, 
p.  353-359. 

Berry,  R.W.,  and  Fischer,  P. J.,  1978,  Clay  mineral  distribution  and 
oceon  currents:  southern  California  borderland:  Geological  Soci- 
ety of  America  Abstracts  with  Programs,  v.   10,  p.  96. 

Beyer,  L.A.,  1979,  Geologicol  and  geophysical  implications  of  den- 
sity and  sonic  logs,  in  Cook,  H.E.,  editor.  Geologic  studies  of  the 
Point  Conception  deep-strotigrophic  test  well  OCS-CAL  78-164 
No.  1,  outer  continental  shelf,  southern  California,  United  States: 
U.S.  Geological  Survey  Open-File  Report  79-1218,  p.  59-70 

Beyer,  L.A.,  1980,  Offshore  southern  California,  in  Oliver,  H.W., 
editor.  Interpretation  of  the  gravity  map  of  Californio  and  its 
continental  margin:  California  Division  of  Mines  ond  Geology 
Bulletin  205,  p.  815. 

Beyer,  L.A.,  and  Biehler,  S.,  1981,  Bouguer  gravity  mop  of  Califor- 
nia, Long  Beach  sheet:  Californio  Division  of  Mines  ond  Geology, 
scale  1:250,000. 

Beyer,  L.A.,  and  Biehler,  S.,  1982,  Bouguer  gravity  mop  of  Califor- 
nia, Long  Beach  sheet:  California  Division  of  Mines  and  Geology, 
1  sheet,  scale  1:250,000. 

Beyer,  L.A.,  and  Rietmon,  J.D.,  1982,  Bouguer  gravity  mop  of  Cali- 
fornia, Sonto  Mario  sheet:  California  Division  of  Mines  and  Ge- 
ology, scale  1:250,000. 

Beyer,  L.A.,  Sosnett,  N.B.,  and  Pisciotto,  K.A.,  1975,  Interpretations 
of  gravity  and  magnetic  surveys  of  California  continental  border- 
land (abstract):  Program  50th  Annual  Pacific  Section  Meeting, 
Americon  Association  of  Petroleum  Geologists,  SEPT-SEG. 

Bickmore,  O.K.,  1967,  Offshore-onshore  petroleum  study,  Sonto  Bar- 
bora  Channel — phase  I,  effects  of  federal  leasing,  outer  conti- 
nental shelf  unpublished  preliminary  report:  Oil  Well  Inspection 
Department,  Sonto  Borboro  County,  California,  159  p. 

Bird,  C.V.,  1978,  Estimoted  oil  and  gas  reserves,  southern  Californio 
outer  continental  shelf,  January  1,  1977:  U.S.  Geological  Survey 
Open-File  Report  78-384,  p.  9. 

Bird,  C.V.,  1980,  Estimated  oil  and  gas  reserves,  southern  California 
outer  continental  shelf,  January  1,  1979:  U.S.  Geological  Survey 
Open-File  Report  80-477,  10  p. 

Birdsoll,  B.C.,  ond  Scott,  R.N.M.,  1976,  Physical  ond  biogenic  char- 
acteristics of  sediments  from  upper  Hueneme  submarine  canyon 
California  coast:  American  Association  of  Petroleum  Geologists 
Bulletin,  V.  60,  p.  650. 

Birkelond,  P.W.,  1972,  Lote  Quoternory  eustatic  seo  level  changes 
along  Molibu  coast,  Los  Angeles  County,  California:  Journal  of 
Geology,  v.  80,  p.  432-448. 

Bishop,  C.C,  ond  Chopman,  R.H.,  1967  (revised  1980),  Bouguer 
gravity  mop  of  Colifornio,  Sonto  Cruz  sheet:  California  Division 
of  Mines  ond  Geology,  scale  1:250,000. 

Bloke,  G.H.,  1977,  Distribution  and  temporal  migration  of  bank  top 
foraminifera  assemblages,  outer  southern  California  borderland: 
Americon  Association  of  Petroleum  Geologists  Bulletin,  v.  61,  p. 
76«  767. 

Bloke,  M.C.,  Jr.,  Compbell,  R.H.,  Dibblee,  T.W.,  Jr.,  Howell,  D.G., 
Nilsen,  T.H,,  Normark,  W.R.,  Vedder,  J.G.,  and  Silver,  E.A., 
1978,  Neogene  basin  formotion  in  relation  to  plate-tectonic  evo- 
lution of  the  San  Andreas  fault  system,  Colifornio:  American 
Association  of  Petroleum  Geologists  Bulletin,  v.  62,  p.  344-372. 

Bloke,  M.C.,  Jr.,  Howell,  D.G.,  and  Jones,  D.L.,  1982,  Preliminary 
tectonostrotigrophic  terrone  mop  of  California:  U.S.  Geological 
Survey  Open  File  Report  82-593. 

Blake,  M.C.,  Jr.,  Jones,  D.L.,  and  Landis,  C.H.,  1974,  Active  continen- 
tal margins:  contrasts  between  Californio  ond  New  Zealand,  in 


76 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


Burk,  C.A.,  ond  Drake,  C.L.,  editors,  The  geology  of  confinentol 
morgins:  SpringerVerlog,  p.  853-872. 

Bloke,  W.,  1855,  Observations  on  the  physical  geography  and  geol- 
ogy of  the  coast  of  California,  from  Bodega  Boy  to  Son  Diego; 
U.S.  Coost  ond  Geodetic  Survey  Annual  Report,  no.  65,  p.  376- 
398. 

Bloom,  L.,  Smith,  D.R.,  and  Osborne,  R.H.,  1979,  Examination  of 
sand  transport  from  the  Santa  Clara  River  wotershed  through  the 
southern  Santa  Borboro  littoral  cell  by  means  of  groin  surface 
microtextures  and  Fourier  grain  shape  analysis:  Geological  Soci- 
ety of  Americo  Abstracts  with  Programs,  v.  11,  p.  71. 

Bogaert,  B.,  Reichle,  M.,  Prothero,  W.,  and  Zelikovitz,  S.,  1978, 
Aftershock  study  of  the  August  13,  1978  Santo  Barbara,  Colifor- 
nio  earthquake:  American  Geophysical  Union  Tronsoctions  Ab- 
stract, V.  59,  p.   1130. 

Bolt,  B.A.,  Lomnitz,  C,  and  McEvilly,  T.V.,  1968,  Seismological  evi- 
dence on  the  tectonics  of  central  and  northern  California  and  the 
Mendocino  escarpment:  Bulletin  of  the  Seismological  Society  of 
Americo,  v.  58,  p.  1725-1767. 

Boore,  D.M.,  and  Stierman,  D.J.,  1973,  Source  porameters  of  the 
Point  Mugu,  California,  earthquake  of  February  21,  1973:  Bulle- 
tin of  the  Seismological  Society  of  America,  v.  66,  p.  385-404. 

Booth,  J.S.,  1971,  Sediment  dispersion  in  northern  Channel  Island 
passages,  California  continental  borderland:  University  of  South- 
ern Colifornia  unpublished  Master's  Thesis. 

Booth,  J.S.,  1973,  Early  diagenesis  in  southern  California  continental 
borderlond  sediments:  University  of  Southern  California  unpub- 
lished Doctoral  Thesis. 

Booth,  J.S.,  1973,  Textural  changes  as  on  indicator  of  sediment 
dispersion  in  the  northern  Channel  Island  passages,  California: 
Journol  of  Sedimentary  Petrology,  v.  43,  p.  238-250. 

Booth,  J.S.,  1974,  Eorly  diagenesis  in  southern  California  continental 
borderland  sediments:  Dissertation  Abstracts,  v.  35,  p.  319B- 
320B. 

Booth,  J.S.,  and  Sangrey,  D.A.,  1979,  Mass  movement  potential  of 
recent  sediments  on  the  United  States  continental  morgins:  Geo- 
logical Society  of  America  Abstracts  with  Programs,  v.  11,  p. 
391. 

Borchardt,  R.D.,  Gibbs,  J.F.,  ond  Lojoie,  K.R.,  1975,  Prediction  of 
maximum  earthquake  intensity  in  the  Son  Francisco  Bay  region, 
Colifornia,  for  large  earthquakes  on  the  San  Andreas  and  Hoy- 
word  faults:  U.S.  Geologicol  Survey  Miscellaneous  Field  Studies 
Mop  MF-709,  1:125,000,  3  sheets. 

Bottjer,  D.J.,  ond  Link,  M.H.,  1984,  A  synthesis  of  lote  Cretaceous 
southern  California  and  northern  Bajo  California  Poleogeogro- 
phy,  in  Crouch,  J.K.,  and  Bochmon,  SB.,  editors.  Tectonics  ond 
sedimentation  along  the  California  margin:  Society  of  Economic 
Paleontologists  and  Mineralogists,  Pacific  Section,  v.  38,  p.  171- 
188. 

Bowers,  S.,  1878,  Geology  at  Sonto  Rosa  Islond:  Smithsonian  Insti- 
tute Annuol  Report  for  1877,  p.  316-320. 

Bowers,  S.,  1890,  Son  Nicolas  Island:  Colifornio  State  Mineralogist 
Ninth  Annual  Report,  p.  57-61. 

Brodner,  H.,  Legg,  M.R.,  and  Reichle,  M.S.,  1970,  Sonobuoy  meas- 
urement of  aftershocks  of  Santo  Barbara  13  August  1973  earth- 
quake: Americon  Geophysical  Union  Transactions  Abstracts,  v. 
59,  p.  1130. 

Bremner,  C.  St.  J.,  1932,  Geology  of  Santo  Cruz  Island,  Santa 
Barbara  County,  California:  Santo  Borboro  Museum  of  Natural 
History,  Occasional  Papers,  v.  1,  p.  33. 

Bremner,  C.  St.  J.,  1933,  Geology  of  San  Miguel  Island,  Santa 
Barbara  County,  California:  Santo  Barbara  Museum  of  Noturol 
History,  Occasional  Popers,  v    3,  p.  23. 

Bromery,  R.W.,  Emery,  K.O.,  and  Bolsey,  JR..  Jr.,  1960,  Reconnais- 
sance airborne   magnetometer   survey   off   southern   California: 


U.S.  Geologicol  Survey,  Geophysical  Investigations  Mop,  GP 
211. 

Brooks,  R.A.,  1973,  A  bottom  gravity  survey  of  the  shallow  water 
regions  of  southern  Monterey  Bay  and  its  geological  interpreto- 
tion:  U.S.  Novol  Postgraduate  School,  Monterey,  California, 
M.S.  Thesis,  92  p.;  ovailoble  from  Notional  Technical  Information 
Service,  U.S.  Department  of  Commerce,  Springfield,  Virginia, 
NTIS-A761-472. 

Brown,  R.D.,  1972,  Faults  that  are  historically  active  or  that  show 
evidence  of  geologically  young  surface  displacement,  San  Fron- 
cisco  Bay  region,  a  progress  report:  October  1970:  U.S.  Geologi- 
cal Survey  Miscellaneous  Field  Studies  Map  331,  scale 
1:250,000. 

Brown,  R.D.,  Jr.,  and  Wolfe,  E.W.,  1973,  Mop  showing  recently 
active  breaks  along  the  Son  Andrcos  fault  between  Point  Del- 
godo  and  Bolinos  Bay,  California:  U.S.  Geological  Survey  Mis- 
celloneous  Investigation  692,  scole  1:24,000. 

Brown,  W.M.,  III,  1974,  Sediment  sources  and  deposition  sites  and 
erosionol  and  depositionol  provinces,  Marin  and  Sonoma  coun- 
ties, California:  San  Francisco  Boy  Environment  and  Resources 
Planning  Study,  Interpretative  Report  7,  U.S.  Department  of  the 
Interior,  Geological  Survey — U.S.  Deportment  of  Housing  ond 
Urban  Development. 

Brown,  W.M.,  III,  ond  Jackson,  L.E.,  Jr.,  1973,  Erosionol  and  deposi- 
tionol provinces  and  sediment-transport  in  the  south  cenfrol  Son 
Francisco  Boy  region,  California:  Son  Francisco  Boy  Environment 
and  Resources  Plonning  Study,  Interpretative  Report  3,  U.S.  De- 
partment of  the  Interior,  Geological  Survey — U.S.  Department  of 
Housing  and  Urban  Development. 

Brown,  W.M.,  III,  and  Jackson,  L.E.,  Jr.,  1973,  Preliminary  map  of 
erosionol  and  depositionol  provinces  and  description  of  sedi- 
ment-tronsport  processes  in  the  south  central  Son  Froncisco  Bay 
region,  California:  U.S.  Geological  Survey  Miscellaneous  Field 
Studies  Mop  515,  scale  1:125,000,  p.  21. 

Brown,  W.M.,  III,  and  Ritter,  J.M.,  1971,  Sediment  transport  and 
turbidity  in  the  Eel  River  Basin,  Colifornio:  U.S.  Geological  Sur- 
vey Woter  Supply  Poper  1986,  p.  70. 

Bruff,  S.C,  1940,  The  Pleistocene  history  of  the  Newport  Bay  area, 
southern  California:  University  of  California,  Berkeley,  unpub- 
lished Moster's  Thesis. 

Brunner,  C.A.,  and  Normork,  W.R.,  in  press,  Biostratigraphic  implica- 
tions for  turbidite  depositionol  processes  of  the  Monterey  deep- 
sea  fan,  centrol  California,  Journal  of  Sedimentory  Petrology 
(Director's  approval  2  July  1984). 

Buchonon-Bonks,  J.M.,  Pompeyon,  E.H.,  Wagner,  H.C.,  ond  McCul- 
loch,  D.S.,  1978,  Preliminory  mop  showing  recency  of  faulting  in 
coostol  soufh-centrol  Colifornia,  U.S.  Geological  Survey  Map 
MF-910,  scale  1:250,000. 

Bufe,  C.G.,  Lester,  F.W.,  Meagher,  K.L,  and  Wesson,  R.L.,  1975, 
Catolog  of  earthquakes  along  the  Son  Andreas  fault  system  in 
central  California,  April  -  June,  1973:  U.S.  Geologicol  Survey 
Open-File  Report  75-125,  44  p. 

Buffington,  E.C.,  1951,  Gullied  submorine  slopes  off  southern  Cali- 
fornia: Geological  Society  of  America  Bulletin,  v.  62,  p.   1497. 

Buffington,  E.C,  1952,  Natural  Levees:  Journal  of  Geology,  v.  60, 
p.  473-479. 

Buffington,  E.C,  1964,  Structural  control  and  precision  bathymetry 
of  Lo  Jollo  submorine  canyon,  California:  Marine  Geology,  v.  1, 
p.  44  58. 

Buffington,  EC,  ond  Moore,  D.G.,  1963,  Geophysical  evidence  on 
the  origin  of  gullied  submarine  slopes.  Son  Clemente,  California: 
Journal  of  Geology,  v.  71,  p.  356-370. 

Buiko,  J. A.,  and  Teng,  T.,  1979,  A  seismicity  study  for  portions  of 
the  Los  Angeles  basin,  Santo  Monica  basin,  and  Santa  Monico 
mountains,  California:  University  of  California,  Geophysics  Labo- 
ratory, Technical  Report  79-9,  191  p. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


77 


Bukry,  J.D.,  and  Crouch,  J.K.,  1979,  Planktonic  microfossils  and  the 
lower-middle   Miocene  boundory  in  the  Californio  borderland: 
U.S.  Geological  Survey  Professional  Poper  1150. 
Bukry,  J.D.,  ond  Kennedy,  M.P.,  1969,  Cretaceous  and  Eocene  coc- 
coliths  at  San  Diego,  California,  in  Short  contributions  to  Califor- 
nia Geology:  California  Division  of  Mines  and  Geology  Special 
Report  100,  p.  33-43. 
Bunnell,  V.A.,   1969,  The  woter  structure  of  the  San  Pedro  basin, 
California  borderland;  University  of  Southern  California  unpub- 
lished Master's  Thesis. 
Burk,  C.A.,  ond  Moores,  E.M.,  1968,  Problems  of  major  faulting  at 
continental  margins,  with  special  reference  to  the  San  Andreas 
fault  system,  in  Dickinson,  W.R.,  and  Grantz,  A.,  editors.  Pro- 
ceedings of  conference  on  geologic  problems  of  Son  Andreas 
fault    system:     Stanford     University     Publications,     Geological 
Sciences,  v.  11,  p.  358-374. 
Burnhom,  W.L.,  Kunkel,  F.,  Hufmann,  W.,  and  Peterson,  W.C,  1963, 
Hydrogeologic  reconnaissance  of  Son  Nicolas  Island,  Californio: 
U.S.  Geological  Survey  Woter-Supply  Paper  1539-0,  p.   1-43. 
Butcher,  W.S.,    1951,   Foraminifero,  Coronado  Bonk  and  vicinity, 
California:  University  of  California,  Scripps  Institution  of  Ocean- 
ography, Submarine  Geology  Report  19,  p.  1-9. 
Butcher,  W.S.,   1951,   Lithology  of  the  offshore  San  Diego  area: 
University  of  California,   Scripps  Institution  of  Oceonogrophy, 
Submarine  Geology  Report  20,  8  p. 
Butcher,  W.S.,   1951,   Lithology  of  the  offshore  San  Diego  oreo, 
Colifornio:  University  of  Californio,  Scripps  Institution  of  Oceanog- 
raphy unpublished  Doctoral  Thesis. 
Byerly,  P,  1930,  The  Californio  earthquake  of  November  4,  1927: 

Seismological  Society  of  America  Bulletin,  v.  20,  p.  53-66. 
Byerly,  P.,  1937,  Earthquakes  off  the  coast  of  northern  California: 

Seismologicol  Society  of  America  Bulletin,  v.  27,  p.  73-96. 
Cacchione,  D.A.,  Drake,  D.E.,  Clarke,  S.H.,  and  Masson,  D.G.,  1984, 
Long-ronge   side-scon-sonor  studies  of   the  northern   Californio 
and  southern  Oregon  EEZ:  Geological  Society  of  America  Ab- 
stracts with  Programs,  v.  16,  no.  6,  p.  461. 
Cacchione,  D.A.,  Drake,  D.E.,  Clarke,  S.H.,  ond  Masson,  D.G.,  1984, 
Physiography  of  the  seafloor  off  northern  California  and  south- 
ern Oregon:   EOS,  Transactions  of  the  Americon  Geophysical 
Survey  Bulletin  1645,  101  p.,  27  figures. 
Cacchione,  D.A.,  and  EEZ-SCAN  '84  Scientific  Team  (Drake,  D.E., 
Edwards,  B.D.,  Field,  M.E.,  Gardner,  J.V.,  Hampton,  M.A.,  Korl, 
H.A.,  and  McCulloch,  D.S.) ,  1984,  GLORIA  II  sonogroph  mosaic 
of  the  western  U.S.  Exclusive  Economic  Zone,  EOS,  Tronsactions 
of  the  Americon  Geophysical  Union,  7  p. 
Cacchione,  DA.,  Drake,  D.E.,  Dingier,  J.R.,  Winont,  CD.,  and  Ol- 
son, J.R.,   1976,  Observolions  of  sediment  transport  by  surface 
and  internal  waves  off  Son  Diego,  California:  American  Geo- 
physical Union  Transactions,  v.  58,  p.  307. 
Cacchione,  D.A.,  Karl,  H.A.,  and  Drake,  D.E.,  1980,  Sediment  trons 
port  by   internal   woves   on   the   continentol   shelf   off   southern 
California:  Symposium,  "Sedimentary  Dynamics  of  Continental 
Shelves,"  International  Geological  Congress,  Poris. 
Caldwell,  J.M.,  1956,  Wove  oction  and  sand  movement  near  Ana- 
heim Boy,  California:  U.S.  Army  Corps  of  Engineers,  Beach  Ero- 
sion Boord,  Technical  Memorandum  68,  21   p. 
Cameron,  J.B.,  1961,  Earthquakes  in  the  northern  California  coastal 
region  (port  I) :  Seismological  Society  of  America  Bulletin,  v.  51, 
p.  203-221. 
Comeron,  J.B.,  1961,  Earthqookei  in  the  northern  California  cooital 
region  (part  II) :  Seismological  Society  of  Americo  Bulletin,  v.  51, 
p.  337  354. 
Campbell,  R.H.,  1973,  Generolized  geologic  mop  ond  structure  sec- 
tions, Sonto  Clora  River  to  Sonto  Monica  Boy,  southern  Califor- 
nio, in  Cretocaout  stratigraphy  of  the  Sonto  Monica  Mountains 


and    Simi    Hills:    Society    of    Economic    Paleontologists    and 
Mineralogists,  Pacific  Sections,  Fall  Field  Trip  Guidebook. 

Campbell,  R.H.,  Wolf,  S.C,  Hunter,  R.E.,  Lee,  W.H.K.,  Ellsworth, 
W.L.,  Wogner,  H.C.,  Vedder,  J.G.,  and  Junger,  A.,  1975,  The 
Sonto  Barbara  Channel  region,  o  review:  Geological  Society  of 
America  Abstracts  with  Programs,  v.  7,  p.  301-302. 

Campbell,  R.H.,  Wolf,  S.C,  Hunter,  R.E.,  Wagner,  H.C,  Junger,  A., 
and  Vedder,  J.G.,  1975,  Geologic  mop  and  sections,  Sonto 
Barboro  Channel  region,  California;  U.S.  Geological  Survey 
Open-File  Mop  75-123. 

Campbell,  R.H.,  ond  Yerkes,  R.F.,  1976,  Cenozoic  evolution  of  the 
Los  Angeles  Basin  area;  relation  to  plate  tectonics,  in  Howell, 
D.G.,  editor.  Aspects  of  the  geologic  history  of  the  Colifornio 
continentol  borderland;  American  Association  of  Petroleum 
Geologists,  Pacific  Section,  Miscellaneous  Publication  24,  p.  541- 
558. 

Carius,  T.,  and  Richards,  A.F.,  1976,  Son  Diego  Trough  geotechnicol 
test  area:  Marine  Geotechnology,  Crone,  Russok,  Co.,  New  York, 
V.  1,  p.  345-369. 

Carlson,  P.R.,  ond  McCulloch,  D.S.,  1969,  Bedrock  configuration  of 
central  Son  Francisco  Bay  based  on  continuous  acoustic  profiles; 
Association  of  Engineering  Geologists  Annual  Meeting  Abstract, 
21  p. 

Carlson,  P.R.,  and  McCulloch,  D.S.,  1970,  Bedrock-surface  mop  of 
central  Son  Froncisco  Bay;  U.S.  Geologicol  Survey — U.S.  De- 
partment of  Housing  and  Urban  Development  Basic  Data  Contri- 
bution Number  10,  1   mop  sheet. 

Carlson,  P.R.,  Alpha,  T.R.,  and  McCulloch,  D.S.,  1970,  The  floor  of 
centrol  Son  Francisco  Boy:  California  Division  of  Mines  and  Ge- 
ology, Mineral  Information  Service,  Son  Francisco,  v.  23,  p.  97- 
107. 

Carlson,  P.R.,  and  McCulloch,  D.S.,  1974,  Aeriol  observations  of  the 
suspended-sediment  plumes  in  Son  Francisco  Bay  and  the  odjo- 
cent  Pacific  Ocean:  U.S.  Geological  Survey  Journal  of  Research, 
v.  2,  p.  519-526. 

Carlson,  P.R.,  McCulloch,  D.S.,  Peterson,  D.H.,  and  Castle,  R.W., 
1970,  Comparison  of  ocoustic  reflectors  and  boreline  lithologies: 
Southern  San  Francisco  Boy;  Geological  Society  of  America  Ab- 
stracts with  Programs,  v.  2,  p.  78-79. 

Carlson,  P.R.,  Peterson,  D.H.,  Conomos,  T.J.,  McCulloch,  D.S.,  1970, 
Aerial  and  in  situ  observations  of  o  fresh-water  plume  in  Son 
Froncisco  Boy  and  adjacent  Pacific:  American  Geophysical  Union 
Tronsoctions,  v.  51,  p.  767. 

Corlson,  R.L.,  1981,  Late  Cenozoic  rotation  of  the  Juan  de  Fuco 
Ridge  and  the  Gordo  Rise;  A  cose  study;  Tectonophysics,  v.  77, 
p.  171-181. 

Carter,  F.B.,  1954,  Oil  and  gas  production  in  California,  in  Johns, 
R.H.,  editor,  Geology  of  southern  Colifornio:  California  Division 
of  Mines  Bulletin  170,  Chapter  9,  p.  21-28. 

Carter,  L.S.,  1971,  Recent  marine  sediments  of  Carmel  Bay,  Colifor- 
nio; U.S.  Novol  Academy  unpublished  Master's  Thesis. 

Casey,  R.E.,  1972,  Neogene  rodiolarion  biostrotigrophy  ond  poleo- 
temperotures;  southern  Californio,  the  experimentol  Mohole, 
Antarctic  core  E  14-8;  Poleogeogrophy,  Poleoclimotology,  Poleo- 
ecology:  on  Internotionol  Journal  for  the  Geo- Sciences,  Elsevier 
Publicotion  Company,  Amsterdam,  v.   12,  p.   115-130. 

Cosey,  RE.,  ond  Price,  A  B.,  1973,  A  tentative  rodiolarion  zonation 
and  paleo  oceonographic  interpretation  from  Newport  Boy,  Col 
Ifornio:  Society  of  Economic  Paleontologists  ond  Minerologisis, 
Pocific  Section  Guidebook,  p.  67-70. 

Caster,  W.A.,  1969,  Near-bottom  currents  in  Monterey  submorine 
canyon  and  on  the  adjacent  continental  shelf:  U.S.  Novol  Acade- 
my unpublished  Mosler's  Thesis. 

Castro.  M.J.,  1966.  Sonto  Borbaro  Chonnel  potential:  Oil  ond  Gas 
Journal,  v.  64,  p.  98  105 


78 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


Chomberloln,  T.K.,  1964,  Moss  transport  of  sediment  in  the  heads 
of  Scripps  submarine  canyon,  California,  in  Miller,  R.L.,  editor. 
Marine  geology,  Shepord  commemorative  volume,  MacMillon, 
New  York,  p.  42-64. 

Cheney,  R.W.,  and  Mason,  H.L.,  1930,  A  Pleistocene  flora  from 
Santo  Cruz  Island,  California:  Carnegie  Institute,  Washington,  p. 
1-24. 

Chapman,  R.H.,  1966,  Gravity  base  station  network:  California  Divi- 
sion of  Mines  and  Geology  Special  Report  90,  49  p. 

Chopman,  R.H.,  and  Bishop,  C.C.,  1968,  Bouguer  gravity  mop  of 
California,  San  Francisco  sheet:  California  Division  of  Mines  and 
geology,  scole  1:250,000. 

Chase,  C.G.,  Menard,  H.W.,  Larson,  R.L.,  Sharman,  G.F.,  III,  and 
Smith,  S.M.,  1970,  History  of  sea-floor  spreading  west  of  Bojo 
California:  Geological  Society  of  America  Bulletin,  v.  18,  no.  2, 
p.  491-498. 

Chase,  T.E.,  Normark,  W.R.,  and  Thomas,  J. A.,  1979,  Compilation 
of  marine  geologic  and  oceanographic  data  off  the  western 
United  States:  southern  California  continental  borderland:  Geo- 
logical Society  of  America  Abstracts  with  Programs,  v.  11,  p. 
400. 

Chose,  T.E.,  Wilde,  P.,  and  Normark,  W.R.,  1975,  Oceanographic 
data  of  the  Monterey  deep-sea  fan:  University  of  California,  Son 
Diego,  Institute  of  Marine  Resources  Technical  Report,  Series 
TR-58. 

Chestermon,  C.W.,  1952,  Descriptive  petrography  of  rocks  dredged 
off  the  coost  of  central  California:  California  Academy  of 
Sciences  Proceedings,  v.  27,  p.  359-374. 

Christodoulidis,  D.C.,  Smith,  D.E.,  Minster,  J.B.,  and  Jordan,  T.H., 
1985,  Relative  movement  at  tectonic  plates  in  California  ob- 
served by  satellite  laser  ranging:  Science    (in  press). 

Clark,  J.C,  Brabb,  E.E.,  Greene,  H.G.,  and  Ross,  D.C.,  1984,  Geol- 
ogy of  Point  Reyes  Peninsula  and  implications  for  San  Gregorio 
fault  history,  in  Crouch,  J.K.,  and  Bochmon,  S.B.,  editors.  Tecton- 
ics and  sedimentation  along  the  California  margin:  Society  of 
Economic  Paleontologists  and  Mineralogists,  Pocific  Section,  v. 
38,  p.  67-86. 

Clark,  J.T.,  1944,  Index  to  descriptive  catalog  of  earthquakes  of  the 
Pacific  coost  of  the  United  States,  1769-1928:  Seismologicol 
Society  of  America  Bulletin,  v.  34,  p.  35-62. 

Clarke,  S.  H.,  1987,  Geology  of  the  California  continental  margin 
north  of  Cape  Mendocino,  in  Scholl,  D.  W.,  Grontz,  A.,  and 
Vedder,  J.G.,  editors.  Geology  and  resource  potential  of  the 
continental  margin  of  western  North  America  and  adjacent 
ocean  basins — Beaufort  Sea  to  Bojo  California:  Circum  Pacific 
Council  for  Energy  and  Mineral  Resources,  Earth  Science  Series 
(in  press) . 

Clorke,  S.H.,  Greene,  H.G.,  Field,  M.E.,  and  Lee,  W.H.K.,  1983, 
Reconnaissance  geology  and  geologic  hazards  of  selected  areas 
of  the  southern  California  continental  borderland:  U.S.  Geologi- 
col  Survey  Open-File  Report  83-62,  78  p.,  5  figures,  18  map 
sheets. 

Clarke,  S.H.,  Greene,  H.G.,  Field,  M.E.,  Lee,  W.H.K.,  and  McCrory, 
PA.,  1980,  Preliminary  report  on  the  environmentol  geology  of 
selected  areas  of  the  southern  California  continental  borderland 
considered  for  OCS  petroleum  lease  sole  48:  Final  Technical 
Report  (U.S.G.S.-B.L.M.  MOU  AA551-MU8-15),  submitted  to 
Pacific  OCS  Office,  Bureau  of  Land  Management,  Februory 
1980,  60  p.,  18  plates. 

Clarke,  S.H.,  Greene,  H.G.,  and  Kennedy,  M.P.,  1985,  Delineating 
active  faults  and  potentially  unstable  slopes  offshore,  in  Ziony, 
J. I.,  editor.  Evaluating  earthquake  hazards  in  the  Los  Angeles 
region — on  earth  science  perspective:  U.S.  Geological  Survey 
Professional  Poper  1360,  p.  347-373. 


Clarke,  S.  H.,  Howell,  D.  G.,  and  Nilsen,  T.  H.,  1975,  Poleogene 
geography  of  California,  in  Weover,  D.  W.,  Hornodoy,  G.  R., 
and  Tipton,  A.,  editors.  Conference  on  future  energy  horizons  of 
the  Pacific  Coast,  Paleogene  symposium  and  selected  technical 
papers:  American  Association  of  Petroleum  Geologists,  Pacific 
Section,  Annual  Meeting,  p.  125-154. 

Cloypool,  G.E.,  and  Kaplan,  I.R.,  1974,  The  origin  of  methane  in 
marine  sediments,  in  Kaplan,  I.R.,  editor,  Noturol  gases  in  marine 
sediments:  Plenum  Press,  New  York,  New  York,  p.  94-129. 

Clements,  T.,  1946,  Some  stages  in  the  geologic  history  of  the 
Channel  Island  region,  southern  California:  Geologic  Society  of 
America  Bulletin,  v.  57,  p.  1250-1251. 

Clements,  T.,  1948,  Terraces  on  Santo  Cotalino  Island,  California: 
Geological  Society  of  America  Bulletin,  v.  59,  p.  1368. 

Clements,  T.,  1955,  The  Pleistocene  history  of  the  Channel  Island 
region,  southern  California,  in  Allen  Hancock  Foundation  for 
Scientific  Research,  Essays  In  the  natural  sciences  in  honor  of 
Captain  Allen  Hancock:  Southern  California  University  Press,  p. 
311-323. 

Clements,  T.,  and  Dono,  S.W.,  1944,  Geologic  significance  of  a 
coarse  marine  sediment  from  near  Santo  Cotalina  Island,  Califor- 
nia: Journal  of  Geology,  v.  52,  p.  351-354. 

Clements,  T.,  and  Emery,  K.O.,  1947,  Seismic  activity  and  topogra- 
phy of  the  sea  floor  off  southern  California:  Seismologicol  Soci- 
ety of  Americo  Bulletin,  v.  37,  p.  307-313. 

Cleveland,  G.B.,  1975,  Landsllding  in  marine  terrace  terrain  Califor- 
nia: California  Division  of  Mines  and  Geology  Special  Report 
119,  24  p. 

Clifton,  H.E.,  Greene,  H.G.,  Moore,  G.W.,  ond  Phillips,  R.L.,  1971, 
Methane  seep  off  Malibu  Point  following  the  Son  Fernando 
earthquake:  U.S.  Geological  Survey  Professional  Paper  733,  p. 
112-116. 

Cockerell,  T.D.A.,  1938,  Son  Miguel  Island,  California:  Scientific 
Monthly,  v.  46,  p.  180-186. 

Cockerell,  T.D.A.,  1939,  Pleistocene  shells  from  San  Clemente  Island, 
California:  Nautilus,  v.  53,  p.  22-23. 

Cockerell,  T.D.A.,  1940,  The  marine  Invertebrate  founo  of  the  Cali- 
fornia Islands:  Pacific  Science  Congress,  6th  Proceedings,  v.  3,  p. 
501-504. 

Cockerhom,  R.S.,  and  Eaton,  J. P.,  1982,  The  Point  Sal,  California 
earthquake  of  May  29,  1980:  Earthquake  Notes,  v.  53,  p.  51. 

Coffmon,  J.L.,  and  Von  Hake,  C.A.,  1973,  Eorthquoke  history  of  the 
United  States:  Notional  Oceanic  and  Atmospheric  Administra- 
tion Publication  41-1,  Washington,  208  p. 

Cohee,  G.V.,  1938,  Sediments  of  the  submarine  canyons  off  the 
California  coast:  Journal  of  Sedimentary  Petrology,  v.  8,  p.  19- 
33. 

Colburn,  I. P.,  1973,  Stratigrophic  relations  of  the  southern  California 
Cretaceous  strata,  in  Cretaceous  stratigraphy  of  the  Santo  Mon- 
ica Mountains  and  SIml  Hills,  southern  California:  Society  of 
Economic  Paleontologists  and  Mineralogists,  Pacific  Section 
Guidebook,  p.  45-73. 

Cole,  J.M.,  1969,  Geology  of  Venture  basin,  California,  os  on  ap- 
proach to  exploration  of  continental  margin:  American  Associa- 
tion of  Petroleum  Geologists  Bulletin,  v.  53,  p.  712. 

Cole,  M.R.,  1970,  Poleocurrent  and  bosin  onolysis  on  Son  Nicolas 
Island,  California:  Ohio  State  University  unpublished  Master's 
Thesis. 

Cole,  M.R.,  1973,  Poleocurrent  and  basin  onolysis  on  Son  Nicolas 
Island,  Callfornio:  Geological  Society  of  America  Abstracts  with 
Programs,  v.  5,  p.  24. 

Cole,  M.R.,  1975,  Eocene  sedimentation  and  poleocurrents,  San 
Nicolas  Island,  California:  Field  Trip  Guidebook,  Cordilleron  Sec- 
tion, Geological  Society  of  America,  71st  Annual  Meeting,  32  p. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


79 


Cole,  M.R.,  1977,  Eocene  paleocurrents  and  sedimentation,  San 
Nicolas  Island,  California:  American  Association  of  Petroleum 
Geologists  Bulletin,  v.  61,  p.  237-247. 

Coloumb,  H.P.,  Jr.,  1972,  Recent  marine  sediments  of  the  central 
California  continental  shelf  between  Point  Lobos  and  Point  Sur: 
U.S.  Naval  Academy  umpublished  Master's  Thesis. 

Cook,  D.O.,  1969,  Sand  transport  in  region  of  shoaling  waters  in  the 
sea  off  southern  California:  American  Association  of  Petroleum 
Geologists  Bulletin,  v.  53,  p.  464-465. 

Cook,  H.E.,  1979,  Geologic  studies  of  Point  Conception  deep  strati- 
graphic  test  well  OCS-Cal  78-164  No.  1,  outer  continental  shelf, 
southern  California,  United  States:  U.S.  Geological  Survey 
Open-File  Report  79-1218,  148  p. 

Cooper,  A.K.,  1971,  Structure  of  the  continental  shelf  west  of  Son 
Francisco,  California:  San  Jose  Stote  University,  unpublished 
Master's  Thesis,  65  p. 

Cooper,  A.,  1973,  Structure  of  the  continental  shelf  west  of  Son 
Francisco,  California:  U.S.  Geological  Survey  Open-File  Report 
73-1907,  65  p. 

Copelin,  E.C.,  1979,  Crude  oil-like  hydrocarbons  in  recent  sediments 
of  Santo  Barbara  basin:  American  Association  of  Petroleum 
Geologists  Bulletin,  v.  63,  p.  436. 

Coppersmith,  K.J.,  and  Griggs,  G.B.,  Morphology,  recent  activity 
and  seismicity  of  the  San  Gregorio  fault  zone,  in  Silver,  E.A.  and 
Normark,  W.R.,  editors,  San  Gregorio-Hosgri  fault  zone,  Califor- 
nia: California  Division  of  Mines  and  Geology  Special  Report 
137,  p.  33-44. 

Corbett,  E.J.,  1984,  Seismicity  and  crustal  structure  studies  of  south- 
ern California:  Tectonic  implications  from  improved  earthquake 
locations:  California  Institute  of  Technology  unpublished  Doc- 
toral Dissertation,  231  p. 

Corbett,  E.J.,  and  Johnson,  C.E.,  1982,  The  Santa  Barbara,  Califor- 
nia, earthquake  of  13  August  1978:  Bulletin  of  the  Seismological 
Society  of  America,  v.  72,  p.  2201-2226. 

Corbett,  E.J.,  and  Piper,  K.A.,  1981,  Santo  Barbara  Island,  Califor- 
nia, earthquake,  September  4,  1981:  American  Geophysical  Un- 
ion Transactions,  v.  62-45,  p.  958. 

Cordova,  S.,  1972,  Cuarta  offshore  oil  field:  California  Division  of 
Oil  and  Gas,  California  Oil  Fields — Summary  of  Operations,  v. 
58,  p.  5-14. 

Corey,  W.H.,  1954,  Tertiary  basins  of  southern  California,  in  Johns, 
R.H.,  editor.  Geology  of  southern  California:  California  Division 
of  Mines  Bulletin  170,  p.  73-83. 

Corey,  W.H.,  1966,  Southern  California  and  offshore  Tertiary  ba- 
sins: American  Association  of  Petroleum  Geologists  Bulletin,  v. 
50,  p.  646. 

Cotton,  C.A.,  1942,  Shorelines  of  transverse  deformation:  Journal  of 
Geomorphology,  v.  5,  p.  45-58. 

Cotton,  M.L.,  1979,  Seasonality  in  benthic  foraminiferol  populations 
of  the  southern  California  borderland:  University  of  Southern 
California  unpublished  Master's  Thesis. 

Cotton,  W.R.,  Hall,  T.N.,  and  Hoy,  E.A.,  1980,  Holocene  behavior 
of  the  Son  Andreas  fault  at  Dogtown,  Point  Reyes  Notional 
Seashore,  California:  U.S.  Geological  Survey  Open-File  Report 
80-1142,  p.  13 

Couch,  R.W.,  1980,  Seismicity  and  crustal  structure  near  the  north 
end  of  the  San  Andreas  fault  system  in  Streitz,  R.  and  Sherburne, 
R.,  editors.  The  Son  Andreas  fault  zone  in  northern  California: 
California  Division  of  Mines  and  Geology  Special  Report  140,  p. 
139-152. 

Crandal,  G.,  Reichle,  M.,  Luyendyk,  B.P.,  and  Prothero,  W.A.,  1979, 
Marine  seismic  refraction  study  of  the  Santa  Barbara  Channel: 
American  Geophysical  Union  Transactions,  v.  60,  p.  886. 

Cronyn,  B.S.,  1973,  Underwater  gravity  survey  of  northern  Monterey 
Bay:  U.S.  Naval  Academy  unpublished  Master's  Thesis. 


Crouch,  J.K.,  1977,  Structure  of  the  outer  California  continental 
borderland  and  a  possible  analogue  in  the  region  between  the 
San  Andreas  and  San  Gabriel  faults:  Geological  Society  of 
America,  Abstracts  with  Programs,  v.  9,  p.  407. 

Crouch,  J.K.,  1979,  Neogene  tectonic  evolution  of  the  California 
continental  borderland  and  western  Transverse  Ranges:  Geologi- 
cal Society  of  America  Bulletin,  v.  90,  p.  338. 

Crouch,  J.K.,  1979,  Marine  geology  and  tectonic  evolution  of  the 
northwestern  margin  of  the  California  continental  borderland, 
University  of  California,  San  Diego,  unpublished  Doctoral  Thesis. 

Crouch,  J.K.,  1979,  Tectonic  history  of  the  outer  part  of  the  Califor- 
nia borderland:  Geological  Society  of  America  Abstracts  with 
Programs,  v.  11,  p.  407. 

Crouch,  J.K.,  1980,  Speculations  on  hydrocarbon  potential  of  deep- 
water  basins  in  outer  southern  California  borderland:  American 
Association  of  Petroleum  Geologists  Bulletin,  v.  64,  p.  440. 

Crouch,  J.K.,  1981,  Northwest  margin  of  California  continental  bor- 
derland: marine  geology  and  tectonic  evolution:  American  As- 
sociation Petroleum  Geologists  Bulletin,  v.  65,  p.  191-218. 

Crouch,  J.K.,  and  Bachman,  S.B.,  editors,  1984,  Tectonics  and  sedi- 
mentation along  the  California  margin:  Society  of  Economic  Pa- 
leontologists and  Mineralogists,  Pacific  Section,  Los  Angeles, 
California,  188  p. 

Crouch,  J.K.,  Bachman,  S.B.,  and  Shay,  J.T.,  1984,  Post-Miocene 
compressional  tectonics  along  the  central  California  margin,  in 
Crouch,  J.K.,  and  Bachman,  S.B.,  editors.  Tectonics  ond  sedimen- 
tation along  the  California  margin:  Society  of  Economic  Paleon- 
tologists and  Mineralogists,  Pacific  Section,  v.  38,  p.  37-54. 

Crouch,  J.K.,  and  Bukry,  D.,  1979,  Comparison  of  Miocene  provincial 
foraminiferol  stages  to  Coccolith  zones  in  the  California  continen- 
tal borderland:  Geology,  v.  7,  p.  211-215. 

Crouch,  J.K.,  and  Bukry,  D.,  1980,  Comparison  of  Miocene  provincial 
foraminiferol  stages  to  Coccolith  zones  in  the  California  continen- 
tal borderland.  Reply:  Geology,  v.  8,  p.  4-5. 

Crouch,  J.K.,  Holmes,  M.L.,  McCulloh,  T.H.,  Long,  A.T.,  and  Brune, 
R.,  1978,  Multichannel  seismic  reflection  and  sonobuoy  refraction 
data  in  the  outer  southern  California  borderland:  U.S.  Geological 
Survey  Open-File  Report  78-706,  3  p. 

Crouch,  R.W.,  1952,  Significance  of  temperature  on  foraminifero 
from  deep  basins  off  southern  California  coast:  American  As- 
sociation Petroleum  Geologists  Bulletin,  v.  36,  p.  807-843. 

Crouch,  R.W.,  1954,  Paleontology  and  paleoecology  of  the  Son 
Pedro  shelf  and  vicinity:  Journal  of  Sedimentary  Petrology,  v.  24, 
p.  182-190. 

Crouch,  R.W.,  and  Poag,  C.W.,  1979,  Amphistegina  gibbosa  d'Or- 
bigny  from  the  California  borderlands:  the  Caribbean  connec- 
tion: Journal  of  Foraminiferol  Research,  v.  9,  p.  85-105. 

Crowe,  B.M.,  Howell,  D.G.,  and  McLean,  H.,  1976,  Miocene  volcanic 
and  volcaniclastic  rocks  of  Santo  Cruz  Island:  evidence  for  offset 
along  the  Santo  Cruz  Island  fault,  in  Fritsche,  A.E.,  TerBest,  H., 
and  Wornordt,  W.W.,  editors,  the  Neogene  symposium:  Society 
of  Economic  Paleontologists  and  Mineralogists,  Pacific  Section, 
San  Francisco,  p.  18. 

Crowe,  B.M.,  McCleon,  H.,  Howell,  D.G.,  and  Higgins,  R.E.,  1976, 
Petrography  and  major-element  chemistry  of  the  Santo  Cruz 
Island  volconics,  in  Howell,  D.G.,  editor.  Aspects  of  the  geologic 
history  of  the  California  continental  borderland:  American  As- 
sociation of  Petroleum  Geologists,  Pocific  Section  Miscellaneous 
Publication  24,  p.  196-215. 

Crowell,  J.C.,  1950,  Submarine  canyons  bordering  southern  Califor- 
nia: Geological  Society  of  America  Bulletin,  v.  61,  p.  1453-1454. 

Crowell,  J.C.,  1952,  Submarine  conyons  bordering  central  and  south- 
ern California:  Journal  of  Geology,  v.  60,  p.  58-83. 

Crowell,  J.C.,  1973,  Origin  of  late  Cenozoic  basins  in  southern 
California:  American  Association  of  Petroleum  Geologists  Bulle- 
tin, V.  57,  774  p. 


80 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


Crowell,  J.C.,  1974,  Origin  of  lote  Cenozoic  basins  in  southern 
California,  in  Dickinson,  W.R.,  editor.  Tectonics  and  sedimenta- 
tion: Society  of  Economic  Paleontologists  and  Mineralogists  Spe- 
ciol  Publication  22,  p.  190-204. 

Crowell,  J.C,  1976,  Implications  of  crustal  stretching  and  shortening 
of  coastal  Ventura  basin,  California,  in  Howell,  D.G.,  editor. 
Aspects  of  the  geologic  history  of  the  California  continental 
borderland:  American  Association  of  Petroleum  Geologists,  Pa- 
cific Section,  Miscellaneous  Publication  24,  p.  365-382. 

Crowell,  J.C,  Beyer,  L.A.,  Biehler,  S.,  Ehlig,  P.L.,  Hall,  E.A.,  Junger, 
A.,  and  Vedder,  J.G.,  1980,  Geologic  cross  sections  from  Patton 
Ridge  to  the  Mojove  Desert,  across  the  Los  Angeles  basin,  south- 
ern California,  in  Maxwell,  J.C,  coordinator:  Contribution  from 
the  plate  morgins  working  group,  U.S.  Geodynamics  Committee, 
Geological  Society  of  America,  map  and  chart  series  MC  28K, 
1:250,000. 

Curran,  J.F.,  1972,  Santo  Barbara  Channel — history  of  offshore 
petroleum  development,  central  Santa  Ynez  Mountains,  Santa 
Barbara  County,  California:  Americon  Association  of  Petroleum 
Geologists  and  Society  of  Economic  Paleontologists  and 
Minerologists,  Pacific  Section  Guidebook,  p.  72-76. 

Curran,  J.F.,  Hall,  K.B.,  and  Herron,  R.F.,  1971,  Geology,  oil  fields, 
and  future  petroleum  potential  of  Santo  Barbara  Channel  area, 
California,  in  Cram,  I.H.,  editor,  Future  petroleum  provinces  of 
the  United  States:  American  Association  of  Petroleum  Geolo- 
gists, Memoir  15,  p.  192-211. 

Curray,  J.R.,  1961,  Late  Quaternary  sec  level — a  discussion:  Geo- 
logical Society  of  America  Bulletin,  v.  72,  no.  11,  p.  1707-1712. 

Curray,  J.R.,  1965,  Late  Quaternary  history,  continental  shelves  of 
the  United  States,  in  Wright,  H.E.,  Jr.,  and  Frey,  D.G.,  editors. 
The  Quaternary  of  the  United  States:  Princeton  University  Press, 
Princeton,  New  Jersey,  p.  723-735. 

Curray,  J.R.,  1965,  Structure  of  the  continental  margin  off  of  central 
California:  New  York  Academy  of  Science  Transcript,  Series  II, 
V.  27,  p.  794-801. 

Curray,  J.R.,  1966,  Geologic  structure  on  the  continental  margin, 
from  subbottom  profiles,  northern  and  central  California:  Califor- 
nia Division  of  Mines  and  Geology  Bulletin  190,  p.  337-342. 

Curray,  J.R.,  1971,  Geology  of  the  continental  margin  off  central 
California:  Report  no.  1971,  submitted  to  the  office  of  marine 
geology   (Contract  no.  14-08-001-11457),  Dec.  1971,  42  p. 

Curray,  J.R.,  and  Nason,  R.D.,  1967,  San  Andreas  fault  north  of 
Point  Arena,  California:  Geological  Society  of  America  Bulletin, 
V.  78,  p.  413-418. 

Curray,  J.R.,  and  Silver,  E.A.,  1971,  Structure  of  the  continental 
margin  ond  distribution  of  basement  rock  types  off  central  Cali- 
fornia: Geological  Society  of  Americo  Abstracts  with  Programs, 
V.  3,  p.  106-107. 

Doetwyler,  C.C,  1966,  Marine  geology  of  Tomales  Boy,  central 
California:  University  of  California,  Scripps  Institution  of  Ocean- 
ography and  Pacific  Marine  Station  Research  Report  No.  6,  169 
P- 

Domosso,  S.P.,  1980,  Polynomorphs  from  Holocene  sediments  of 
basins  in  southern  California  continental  borderland:  American 
Association  of  Petroleum  Geologist  Bulletin,  v.  64,  p.  440. 

Domes  and  Moore,  1978,  Preliminary  geotechnical  investigation  of 
offshore,  beach,  and  seocliff  oreos — proposed  LNG  marine  ter- 
minal near  Point  Conception,  California — report  for  Western 
LNG  Terminal  Associates:  Domes  ond  Moore,  Los  Angeles,  Cali- 
fornia, Job  Nos.  0011  20702  and  0011-209-02. 

Domes  ond  Moore,  ond  Marine  Environmental  Sciences  Associates, 
1983,  Activity  and  earthquake  potenliol  of  the  Polos  Verdes 
foult:  U.S.  Geological  Survey  Final  Technical  Report,  Contract 
Number  1408  0001  19786. 


Davidson,  G.,  1887,  Submarine  volleys  on  the  Pacific  coast  of  the 
United  Stotes:  California  Academy  of  Science  Bulletin,  v.  2,  p. 
265-268. 

Davidson,  G.,  1889,  Pacific  coast — coast  pilot  of  California,  Ore- 
gon, and  Woshingfon:  U.S.  Coast  and  Geodetic  Survey,  U.S. 
Government  Printing  Office,  4th  edition,  721  p. 

Davis,  C.C,  1976,  Observations  of  circulation  and  suspended-sedi- 
ment transport  over  port  of  southern  California  borderland  from 
satellite  imagery:  American  Association  of  Petroleum  Geologists 
Bulletin,  V.  60,  p.  663. 

Davis,  C.C,  1980,  LANDSAT  image  analysis  of  circulation  and  sus- 
pended sediment  transport:  California  continental  borderland: 
University  of  Southern  California,  unpublished  Master's  Thesis. 

Davis,  J.R.,  1971,  Sedimentation  of  Pliocene  sandstones  in  Sonto 
Barbara  Channel,  California:  American  Association  of  Petroleum 
Geologists  Bulletin,  v.  55,  p.  335. 

Day,  P.C,  1977,  Factors  influencing  sediment  distributions  ond  pat- 
terns on  shallow,  high  energy  insular  platform,  northern  Chonnel 
Islands,  California:  American  Association  of  Petroleum  Geolo- 
gists Bulletin,  v.  61,  p.  779. 

Day,  P.C,  and  Doull,  M.E.,  1979,  Geomorphology  of  shallow,  high 
energy  submarine  bonk  tops,  Tanner-Cortes  Bonks,  southern  Cali- 
fornia borderland:  Geological  Society  of  America  Abstracts  witf> 
Programs,  v.   11,  p.  411. 

Dehlinger,  P.,  Couch,  R.W.,  and  Gemperle,  M.,  1967,  Gravity  and 
structure  of  the  eastern  port  of  the  Mendocino  escarpment.  Jour- 
nal of  Geophysical  Research,  v.  72,  p.  1233. 

Dias,  S.A.P.,  1973,  A  bottom  gravity  survey  of  Cormel  Boy,  Colifor- 
nio:  U.S.  Naval  Academy  unpublished  Moster's  Thesis. 

Dickinson,  T.W.R.,  1981,  Plate  tectonics  and  the  continental  margin 
of  California,  in  Ernst,  W.G.,  editor.  The  geotectonic  develop- 
ment of  Californio,  Rubey  v.  1;  Englewood  Cliff,  N.J.,  Prentice- 
Hall,  Inc.,  p.  1-28. 

Dickinson,  W.R.,  Graham,  S.A.,  Ingersoll,  R.V.,  and  Jordan,  T.E., 
1976,  Applications  of  plate  tectonics  to  petroleum  geology  along 
Pacific  margin  of  North  America:  American  Association  of  Petro- 
leum Geologists  Bulletin,  v.  60,  p.  2179. 

Dickinson,  W.R.,  and  Grontz,  A.,  1968,  Proceedings  of  conference 
on  geologic  problems  of  Son  Andreas  fault  system:  Stanford 
University  Publications  in  Geological  Sciences,  v.  11,  374  p. 

Dickinson,  W.R.,  Ingersoll,  R.V.,  and  Graham,  S.A.,  1979,  Poleogene 
sediment  dispersal  and  poleotectonics  in  northern  California: 
Geological  Society  of  America  Bulletin,  Part  1,  v.  90,  p.  897-898. 

Dickinson,  W.R.,  and  Snyder,  W.S.,  1979,  Geometry  of  tripple  func- 
tions related  to  the  Son  Andreas  transform:  Journal  of  Geophysi- 
cal Research,  v.  84,  no.  B2,  p.  561-572. 

Dietz,  R.S.,  1938,  Basins  of  the  sea  floor  off  southern  California: 
Geological  Society  of  America  Proceedings  for  1937,  p.  237. 

Dietz,  R.S.,  Emery,  K.O.,  and  Shepord,  F.P.,  1942,  Phosphorite 
deposits  on  the  sea  floor  off  southern  California:  Geological 
Society  of  America  Bulletin,  v.  53,  p.  815-848. 

Dill,  R.F.,  1964,  Sedimentation  and  erosion  in  Scripps  submarine 
canyon,  in  Miller,  R.L.,  editor.  Papers  in  marine  geology,  Shepord 
Commemorative  volume:  The  Mocmillon  Company,  New  York, 
New  York,  p.  23-41. 

Dill,  R.F.,  1965,  Bothyscoph  observations  in  the  La  Jollo  submarine 
fan  valley:  American  Associotion  of  Petroleum  Geologists  Bulle- 
tin, V.  49,  p.  338. 

Dill,  R.F.,  1967,  Erosion  in  the  head  of  La  Jollo  submarine  canyon, 
in  Seo  level  changes  ond  crustol  movements  of  the  Pacific — 1 1th 
Pacific  Scientific  Congress,  Tokyo,  Symposium  19;  Osaka  City 
University  Journal  of  Geosciences,  v.  10,  p.  105. 

Dill,  R.F.,  1967,  Processes  of  submorine  erosion  in  La  Jollo  fan-volley 
and  their  relotion  to  sediment  distribution  patterns:  Americon 
Association  of  Petroleum  Geologists  Bulletin,  v.  51,  461  p. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


81 


Dill,  R.F.,  1969,  Deeply  submerged  terraces  and  low  sea  cliffs  on  the 
continental  slope  of  southern  California,  Baja  California,  Mexico, 
and  Australia:  Geological  Society  of  America  Special  Paper,  v. 
121,  p.  75-76. 

Dill,  R.F.,  1969,  Pleistocene  sea-level  fluctuations  off  southern  Cali- 
fornia and  their  relation  to  continental  slope  sedimentation: 
American  Association  of  Petroleum  Geologists  Bulletin,  v.  53,  p. 
457-458. 

Dill,  R.F.,  1969,  Earthquake  effects  on  fill  of  Scripps  submarine 
canyon:  Geological  Society  of  America  Bulletin,  v.  80,  p.  321- 
327. 

Dill,  R.F.,  Dietz,  R.S.,  and  Stewart,  H.B.,  1954,  Deep-sea  channels 
and  delta  of  the  Monterey  submarine  canyon:  Geological  Soci- 
ety of  America  Bulletin,  v.  65,  p.  191-194. 

Dingier,  J.R.,  1981,  Stability  of  a  very  coarse-grained  beach  at 
Carmel,  California:  Marine  Geology,  v.  44,  p.  241-252. 

Dodd,  J.R.,  Mead,  J.,  and  Staton,  R.J.,  Jr.,  1977,  Poleomognetic 
strotigrophy  of  Pliocene  Centerville  Beach  section,  northern  Cali- 
fornia: Earth's  Plonetery  Science  Letters,  v.  34,  p.  381-386. 

Dodd,  J.R.,  Mead,  J.,  and  Staton,  R.J.,  Jr.,  1984,  Oxygen  isotopic 
composition  of  Neogene  molluscon  fossils  from  the  Eel  River 
basin  of  California:  Geological  Society  of  America  Bulletin,  v.  95, 
p.  1253-1258. 

Doerner,  D.P.,  1969,  Lower  Tertiary  biostratigraphy  of  southwestern 
Santa  Cruz  Island,  in  Weaver,  D.W.,  ond  others,  editors.  Geol- 
ogy of  the  northern  Channel  Islands:  American  Association  of 
Petroleum  Geologists  and  Society  of  Economic  Paleontologists 
and  Mineralogists,  Pacific  Sections,  Special  Publication,  p.  17- 
29. 

Doerner,  D.P.,  1969,  Poleogene  sequence  in  northern  Channel  Is- 
lands, California:  American  Association  of  Petroleum  Geologists 
Bulletin,  v.  53,  p.  469. 

Dokka,  R.K.,  Harper,  A.S.,  Nardin,  T.R.,  and  Scheidemann,  R.C.,  Jr., 
1978,  High  frequency  magnetic  anomalies  and  mognetite  con- 
centrations beneath  the  Santo  Monica  and  San  Pedro  shelves, 
California  continental  borderland:  Geological  Society  of  Ameri- 
ca Abstracts  with  Programs,  v.  10,  p.  390. 

Dott,  R.G.,  Jr.,  1963,  Dynamics  of  subaqueous  gravity  depositional 
processes:  American  Association  of  Petroleum  Geologists  Bulle- 
tin, V.  47,  p.  104-128. 

Douglas,  R.G.,  1981,  Poleoecology  and  continental  margin  basins: 
A  modern  case  history  from  the  borderland  of  southern  Califor- 
nia, in  Douglas,  R.G.,  Colburn,  I. P.,  and  Gorsline,  D.S.,  editors, 
Depositional  systems  of  active  continental  margin  basins:  Society 
of  Economic  Paleontologists  and  Mineralogists,  Pacific  Section, 
Los  Angeles,  p.  121-156. 

Douglas,  R.G.,  Cotton,  M.L.,  and  Wall,  L.S.,  1978,  Ecologic  patterns 
in  benthic  foraminiferal  populations  in  the  southern  California 
borderland:  Geological  Society  of  America  Abstracts  with  Pro- 
grams, V.  10,  p.  391. 

Douglas,  R.G.,  and  Heitman,  H.L.,  1978,  Slope-basin  benthic  foromi- 
nifero  of  California  borderland:  American  Association  of  Petro- 
leum Geologists  Bulletin,  v.  62,  p.  510. 

Douglas,  R.G.,  and  Heitman,  H.L.,  1979,  Slope  and  basin  benthic 
forominifera  of  the  California  borderland,  in  Doule,  L.J.,  and 
Pilkey,  O.H.,  editors.  Geology  of  continental  slopes:  Society  of 
Economic  Paleontologists  and  Mineralogists  Special  Publication 
27,  p.  231-246. 

Douglas,  R.G.,  Liestman,  J.,  and  Cotton,  M.L.,  1979,  Benthic  foromi- 
nifera as  indicators  of  sediment  transport  in  the  California  bor- 
derland: Geological  Society  of  America  Abstracts  with  Programs, 
V.  11,  p.  415. 

Doyle,  L.J.,  1971,  Investigations  in  the  southern  continental  border- 
land off  California  and  Baja  California:  National  Coastal  Shal- 
low Water  Resources  Conference,  Abstract,  p.  57. 


Doyle,  L.J.,  1971,  Some  tectonic  implications  of  structure  and  lithol- 
ogy  of  the  continental  borderland  between  29  degrees  N  and  32 
degrees  N:  Geological  Society  of  America  Abstracts  with  Pro- 
grams, V.  3,  p.  549. 

Doyle,  L.J.,  1971,  29  degrees  30'N  to  32  degrees  N:  hole  in  the 
southern  California  borderland:  Geological  Society  of  America 
Abstracts  with  Programs,  v.  3,  p.  112. 

Doyle,  L.J.,  1975,  Lithology  structure  and  tectonism  of  the  Baja 
California  continental  borderland,  Mexico:  Geological  Society  of 
America  Abstracts  with  Programs,  v.  7,  p.  312. 

Doyle,  L.J.,  1979,  Anomalously  thick  sediments  in  gaps  in  the  escarp- 
ment type  continental  slopes  of  the  California  borderland  and  the 
west  Florida  margin:  Geological  Society  of  America  Abstracts 
with  Programs,  v.  11,  p.  415. 

Doyle,  L.J.,  and  Bandy,  O.L.,  1972,  Southern  continental  borderland, 
Baja  California:  Its  tectonic  and  environmental  development: 
Geological  Society  of  America  Bulletin,  v.  83,  p.  3785-3794. 

Doyle,  L.J.,  and  Gorsline,  D.S.,  1977,  Marine  geology  of  Baja  Cali- 
fornia continental  borderland,  Mexico:  American  Association  of 
Petroleum  Geologists  Bulletin,  v.  61,  p.  903-917. 

Drake,  D.E.,  1972,  Distribution  and  transport  of  suspended  matter, 
Santo  Barbara  Channel,  California:  University  of  Southern  Cali- 
fornia, unpublished  Doctoral  Thesis. 

Drake,  D.E.,  Cocchione,  D.A.,  and  Karl,  H.A.,  1980,  Offshore  trans- 
port of  suspended  matter  in  the  bottom  water  on  San  Pedro  shelf, 
California:  American  Geophysical  Union  Transactions,  v.  61,  p. 
1000. 

Drake,  D.E.,  and  Kolpack,  R.L.,  1971,  Sediment  transport  on  the 
Ventura  shelf,  Santo  Barbara  Channel,  California:  Geological 
Society  of  America  Abstracts  with  Programs,  v.  3,  p.  549. 

Drake,  D.E.,  Fischer,  P.J.,  and  Kolpack,  R.L.,  1971,  Transport  and 
deposition  of  flood  sediment,  Santa  Barbara  Channel,  California, 
in  Kolpack,  R.L.,  editor.  Biological  and  oceanogrophicol  survey  of 
the  Santo  Barbara  Channel  oil  spill,  1969-1970,  volume  II,  physi- 
cal, chemical,  and  geological  studies:  University  of  Southern 
California,  Sea  Grant  Publication  number  2,  477  p. 

Drake,  D.E.,  and  Gorsline,  D.S.,  1971,  Turbid  layer  distribution  and 
fine-grained  sediment  transport,  Santo  Barbara  Channel,  Califor- 
nia continental  borderland:  Geological  Society  of  America  Ab- 
stracts with  Programs,  v.  3,  p.  112. 

Drake,  D.E.,  Kolpack,  R.L.,  and  Fischer,  P. J.,  Sediment  transport  on 
the  Santa  Barbara  -  Oxnord  shelf,  Santo  Barbara  Channel,  Cali- 
fornia, in  Swift,  D.J. P.,  Duane,  D.B.,  and  Pilkey,  O.H.,  editors. 
Shelf  sediment  transport:  Dowden,  Hutchinson  and  Ross,  Inc., 
Stroudsburg,  Pennsylvania,  p.  307-331. 

Driver,  H.L.,  1948,  Genesis  and  evolution  of  Los  Angeles  basin, 
California:  American  Association  of  Petroleum  Geologists  Bulle- 
tin, V.  32,  p.  109-125. 

Dupre,  W.R.,  1977,  Terraces,  tectonics,  and  climatic  change  in  Mon- 
terey Bay  region,  California:  Geological  Society  of  America  Ab- 
stracts with  Programs,  v.  9,  p.  413-414. 

Dupre,  W.R.,  Clifton,  H.E.,  and  Hunter,  R.E.,  1980,  Modern  sedimen- 
tary facies  of  the  open  Pacific  Coast  and  Pleistocene  analogs 
from  Monterey  Bay,  in  Field,  M.E.,  Bouma,  AH.,  Colburn,  I. P., 
Douglas,  R.G.,  and  Ingle,  J.C.,  editors.  Quaternary  depositional 
environments  of  the  Pacific  coast:  Society  of  Economic  Paleon- 
tologists and  Mineralogists,  Pacific  Section,  Pacific  Coast  Pa- 
leography Symposium  No.  4,  p.  105-120. 

Durham,  J.W.,  1956,  Pacific  coast  Cretaceous  from  Vancouver  Is- 
land to  Bojo  California:  Twentieth  International  Geological  Con- 
gress, Mexico,  Resumenes  de  los  trobojos  presentados, 
supplement  4,  p.  331. 

Eaton,  J.E.,  1933,  Long  Beach,  California,  earthquake  of  March  10, 
1933:  American  Association  of  Petroleum  Geologists  Bulletin,  v. 
17,  p.  732-738. 


82 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


Eaton,  J. P.,  1984,  Focal  mechanisms  of  neor-shore  earthquakes 
between  Santa  Borboro  and  Monterey,  California:  U.S.  Geologi- 
cal Survey  Open-File  Report  84-477,  6  p. 

Edwards,  B.D.,  1977,  Animal-sediment  relationships  in  a  slope  envi- 
ronment: southern  California  continental  borderland:  Geological 
Society  of  America  Abstracts  with  Programs,  v.  9,  p.  415. 

Edwards,  B.D.,  1978,  The  role  of  gravity-induced  and  hemipelagic 
sedimentotion  mechanisms  in  Santa  Cruz  basin,  Colifornio  conti- 
nental borderland:  Geological  Society  of  America  Abstracts  with 
Programs,  v.  10,  p.  395. 

Edwards,  B.D.,  1979,  Animal-sediment  relationships  in  dysoerobic 
bathyal  environments,  California  continental  borderland:  Univer- 
sity of  Southern  Colifornio  Doctoral  Thesis. 

Edwards,  B.D.,  1980,  Lebensspuren  of  dysoerobic,  bathyal  basin, 
California  borderland:  American  Association  of  Petroleum 
Geologists  Bulletin,  v.  64,  p.  703. 

Edwards,  B.D.,  1980,  Mass  movement  effects  on  o  bathyal  mac- 
rofaunal  population,  Colifornio  borderland:  American  Associo- 
tion  of  Petroleum  Geologists  Bulletin,  v.  64,  p.  441-442. 

Edwards,  B.D.,  1982,  Geologic  hazards  in  Santa  Monico  basin:  U.S. 
Geologicol  Survey  Administrative  Report  AA851-IA1-22,  23  p. 

Edwards,  B.D.,  1985,  Bioturbation  in  a  dysoerobic,  bathyal  basin: 
California  borderland,  in  Curron,  H.A.,  editor.  Biogenic  struc- 
tures: their  use  in  interpreting  depositional  environments:  Society 
of  Economic  Paleontologists  and  Mineralogists,  Special  Publica- 
tions, 33  manuscript  pages,  13  figures,  5  plates. 

Edwards,  B.D.,  and  Field,  M.E.,  1980,  Sedimentary  processes  active 
on  slopes  of  the  Colifornio  borderland:  American  Association  of 
Petroleum  Geologists  Bulletin,  v.  64,  p.  442. 

Edwards,  B.D.,  Field,  M.E.,  Carlson,  P.R.,  and  Kenyon,  N.H.,  1984, 
Geomorphic  features  off  southern  California  as  seen  by  the 
GLORIA  side-scon  sonar  system,  in  press:  Annual  Convention 
Americon  Association  of  Petroleum  Geologists,  New  Orleans, 
Morch  24-27. 

Edwards,  B.D.,  Field,  M.E.,  and  Clukey,  EC,  1980,  Geologicol  and 
geotechnicol  analysis  of  a  submarine  slump,  California  border- 
land: 12th  Annual  Offshore  Technology  Conference,  v.  1,  p. 
399-411. 

Edwards,  B.D.,  and  Gorsline,  D.S.,  1978,  New  evidence  of  current 
winnowing  activity  on  Hueneme  Sill,  California  continentol  bor- 
derlond:  Americon  Association  of  Petroleum  Geologists  Bulletin, 
V.  62,  p.  511. 

Edwards,  L.M.,  1967,  Directional  sedimentary  rock  structures,  Mio- 
cene "Modelo"  Formotion,  southwestern  Santa  Cruz  Island,  Coli- 
fornio: Universtiy  of  Colifornio,  Santo  Borboro  unpublished 
Master's  Thesis. 

Elders,  W.A.,  Rex,  R.W.,  Meidov,  T.,  Robinson,  P.T.,  and  Biehler,  S., 
1972,  Crustol  spreading  in  southern  California:  Science,  v.  178, 
p.  15-24. 

Elliott,  W.J.,  1966,  Grovity  survey  and  analysis  of  Son  Diego  em- 
boyment,  southwest  Son  Diego  County,  California:  American 
Association  of  Petroleum  Geologists  Bulletin,  v.  50,  p.  646-647. 

Elliott,  W.J.,  1970,  Gravity  survey  ond  regional  geology  of  the  Son 
Diego  embayment,  southwest  Son  Diego  County,  Colifornio,  in 
Allison,  E.C.,  editor.  Pacific  slope  geology  of  northern  Colifornio 
ond  adjocent  Alto  California:  American  Associotion  of  Petroleum 
Geologists,  Society  of  Economic  Paleontologists  and  Mineralo- 
gists, ond  Society  of  Exploration  Geophysicists,  Pacific  Sections 
Guidebook,  p.  10-22. 

Elsworth,  W.L.,  Campbell,  R.H.,  Hill,  D.P.,  Page,  R.A.,  Alewine,  R.W., 
III,  Honks,  T.C.,  Healon,  T.H.,  Hileman,  J. A.,  Konomori,  H.,  Min- 
ster, B.,  and  Whitcomb,  J.H.,  1973,  Point  Mugu,  California, 
earthquake  of  21  February,  1973  and  its  aftershocks:  Science,  v. 
182,  p.  1127-1129. 


Emery,  K.O.,  1951,  Continental  shelf — southern  Colifornio,  in  Boll, 
M.W.,  editor.  Possible  future  petroleum  provinces  of  North 
Americo:  American  Associotion  of  Petroleum  Geologists  Bulletin, 
V.  35,  p.  249-252. 

Emery,  K.O.,  1952,  Continental  shelf  sediments  of  southern  Califor- 
nia: Geological  Society  of  Americo  Bulletin,  v.  63,  p.  1 105-1 108. 

Emery,  K.O.,  1954,  General  geology  of  the  offshore  area,  southern 
California,  in  Johns,  R.H.,  editor.  Geology  of  southern  Californio: 
California  Division  of  Mines  Bulletin  170,  p.   107-111. 

Emery,  K.O.,  1954,  Source  of  water  in  basins  off  southern  California: 
Journal  of  Marine  Research,  v.  13,  p.  1-21. 

Emery,  K.O.,  1958,  Shallow  submerged  marine  terraces  of  southern 
California:  Geological  Society  of  America  Bulletin,  v.  69,  p.  39- 
60, 

Emery,  K.O.,  1958,  Southern  Colifornio  basins,  in  Weeks,  L.G., 
editor.  Habitat  of  oil:  American  Association  of  Petroleum  Geolo- 
gists, p.  955-967. 

Emery,  K.O.,  1960,  Bosin  ploins  and  aprons  off  southern  California: 
Journal  of  Geology,  v.  68,  p.  464-479. 

Emery,  K.O.,  1960,  The  seo  off  southern  Colifornio,  o  modern  habi- 
tat of  petroleum:  John  Wiley  Sons,  Inc.,  New  York,  New  York, 
366  p. 

Emery,  K.O.,  and  Bray,  E.E.,  1962,  Radiocarbon  dating  of  California 
bosin  sediments:  American  Association  of  Petroleum  Geologists 
Bulletin,  V.  46,  p.  1829-1856. 

Emery,  K.O.,  Butcher,  W.S.,  Gould,  H.R.,  and  Shepord,  F.P.,  1952, 
Submarine  geology  off  Son  Diego,  Colifornio:  Journol  of  Geol- 
ogy, V.  60,  p.  511-548. 

Emery,  K.O.,  ond  Dietz,  R.S.,  1950,  Submarine  phosphorite  deposits 
off  California  and  Mexico:  California  Journol  of  Mines,  v.  46,  p. 
7-15. 

Emery,  K.O.,  and  Hoggon,  D.,  1958,  Gasses  in  morine  sediments: 
American  Association  of  Petroleum  Geologists  Bulletin,  v.  42,  p. 
2174-2188. 

Emery,  K.O.,  and  Hulsemonn,  J.,  1963,  Submarine  canyons  of  south- 
ern California;  Port  I,  Topography,  water,  and  sediments;  Allen 
Hancock  Pacific  Expedition:  University  of  Southern  California 
Press,  V.  27,  80  p. 

Emery,  K.O.,  and  Rittenberg,  S.C,  1952,  Early  diogenesis  of  Califor- 
nia bosin  sediments  in  relation  to  origin  of  oil:  American  Associo- 
tion of  Petroleum  Geologists  Bulletin,  v.  36,  p.  735-806. 

Emery,  K.O.,  and  Shepord,  F.P.,  1945,  Lithology  of  the  sea  floor  off 
southern  California:  Geologicol  Society  of  America  Bulletin,  v. 
56,  p.  431-478. 

Emery,  K.O.,  ond  Terry,  R.D.,  1956,  A  submarine  slope  of  southern 
Californio:  Journal  of  Geology,  v.  64,  p.  271-280. 

Ericson,  D.B.,  Ewing,  M.,  ond  Heezen,  B.C.,  1951,  Deep-sea  sands 
and  submarine  canyons:  Geological  Society  of  Americo  Bulletin, 
V.  62,  p.  961-965. 

Erickson,  J.W.,  1972,  Poleoslope  ond  petrogrophic  onolysis  of  the 
South  Point  Formation,  Sonto  Roso  Island,  Colifornio:  University 
of  California,  Sonto  Borboro,  unpublished  Moster's  Thesis. 

Erickson,  J.W.,  1975,  Sedimentology  of  the  South  Point  Formation 
(Eocene),  Sonto  Roso  Island,  Californio,  in  Weaver,  D.W.,  Hor- 
nodoy,  G.R.,  and  Tipton,  A,  editors.  Future  energy  horizons  of 
the  Pacific  coast:  American  Association  of  Petroleum  Geologists, 
Society  of  Economic  Paleontologists  and  Mineralogists,  ond  Soci- 
ety of  Economic  Geophysicists,  Pacific  Sections,  Poleogene  Sym- 
posium, p.   169  190. 

Erickson,  J.W.,  1975,  Petrology  of  some  middle  ond  lote  Eocene 
sandstones  from  the  southern  Californio  borderland,  in  Weover, 
D.W.,  Hornodoy,  G.R.,  ond  Tipton,  A.,  editors.  Future  energy 
horizons  of  the  Pacific  coost;  American  Associotion  of  Petroleum 
Geologists,  Society  of  Economic  Poleontologists  ond  Minerolo- 
gists,  and  Society  of  Economic  Geophysicists,  Pocific  Sections, 
Poleogene  Symposium,  p.  191-209. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


83 


Euge,  K.M.,  Miller,  C,  and  Palmer,  L.,  1973,  Evidence  for  a  possible 
onshore  extension  of  the  Rose  Canyon  fault  in  the  vicinity  of 
Oceanside,  California:  Geological  Society  of  America  Abstracts 
with  Programs,  v.  5,  p.  39. 

Evenson,  R.E.,  and  Miller,  G.A.,  1963,  Geology  and  ground-water 
feotures  of  Point  Arguello  Naval  Missile  Facility,  Santa  Barbara 
County,  California:  U.S.  Geological  Survey  Water-Supply  Paper 
1619-F,  p.  F1-F35. 

Fabiono,  E.B.,  and  Peddie,  N.W.,  1969,  Grid  values  of  total  mag- 
netic intensity  IGRF-1965:  U.S.  ESSA  Technical  Report  38,  55  p. 

Fairbanks,  H.W.,  1897,  Oscillations  of  the  coast  of  California  during 
the  Pliocene  and  Pleistocene:  American  Geologist,  v.  20,  p.  213- 
245. 

Fan,  P.F.,  1979,  Mineralogy  of  deep-sea  sediments  along  the  Murray 
fracture  zone:  University  of  Hawaii  Press,  Honolulu,  v.  33,  p. 
213-220. 

Felix,  D.W.,  1968,  Economic  evaluation  of  Coronodo  Bank  phos- 
phorite deposit:  University  of  Southern  California,  Department  of 
Geological  Sciences  unpublished  technical  report,  23  p. 

Felix,  D.W.,  1969,  Origin  and  recent  history  of  Newport  submarine 
canyon,  California  continental  borderland:  Technical  Report  for 
Office  of  Naval  Research  Contract  No.  NONR  228  (17),  NR 
083-144,  59  p. 

Felix,  D.W.,  1969,  Origin  and  recent  history  of  Newport  Canyon, 
California  continental  borderland:  University  of  Southern  Califor- 
nia unpublished  Master's  Thesis. 

Felix,  D.W.,  and  Gorsline,  D.S.,  1971,  Newport  submarine  canyon, 
California — an  example  of  the  effects  of  shifting  loci  of  sand 
supply  upon  canyon  position:  Marine  Geology,  v.  10,  p.  177-198. 

Felsher,  Murray,  1969,  The  Santo  Cruz  Canyon  system,  continental 
borderland,  California:  bathymetry  and  texturol  analyses  of  the 
cores:  Geological  Society  of  America  Abstracts  with  Programs, 
V.  2,  p.  63. 

Field,  M.E.,  1976,  Shallow  structure  of  northern  Santa  Rosa  -  Cortes 
Ridge,  southern  California  continental  borderland:  American  As- 
sociation of  Petroleum  Geologists  Bulletin  v.  60,  p.  670. 

Field,  M.E.,  1980,  Off-shelf  sediment  transport  by  slides  and  flows, 
California  continental  margin:  International  Geological  Con- 
gress, Abstract  v.  26,  Paris  1980. 

Field,  M.E.,  1981,  Sediment  mass  transport  in  basins:  controls  and 
patterns,  in  Douglas,  R.G.,  Colburn,  I.P.,  and  Gorsline,  D.S., 
editors,  Depositionol  systems  of  active  continental  margins;  Short 
course  notes:  Society  of  Economic  Paleontologists  and  Mineralo- 
gists, Pacific  Section,  Los  Angeles,  p.  61-84. 

Field,  M.E.,  and  Clarke,  S.H.,  Jr.,  1977,  Submarine  slumps  and 
sediment  flows  off  San  Nicolas  Island,  southern  California: 
American  Association  of  Petroleum  Geologists  Bulletin,  v.  61,  p. 
783. 

Field,  M.E.,  and  Clarke,  S.H.,  Jr.,  1979,  Small-scale  slumps  and  slides 
and  their  significance  for  basin  slope  processes,  southern  Califor- 
nia borderland,  in  Doyle,  L.J.,  and  Pilkey,  O.H.,  editors.  Geology 
of  continental  slopes:  Society  of  Economic  Paleontologists  and 
Mineralogists  Special  Publication  27,  p.  223-230. 

Field,  M.E.,  Clarke,  S.H.,  Jr.,  and  Greene,  H.G.,  1977,  Evaluation  of 
geologic  hazards  in  outer  continental  shelf  petroleum  lease 
areas,  southern  California  continental  borderland:  Offshore 
Technology  Conference,  Poper  number  2736,  Proceedings  vol- 
ume 1,  p.  67-78. 

Field,  M.E.,  Clarke,  S.H.,  Jr.,  Greene,  H.G.,  Molnio,  B.F.,  Carlson, 
P.R.,  Hampton,  M.A.,  and  Boumo,  A.H.,  1978,  Seafloor  instabili- 
ty on  Pacific  continentol  margins:  American  Association  of  Petro- 
leum Geologists  Bulletin,  v.  62,  p.  1216-1217. 

Field,  M.E.,  Clarke,  S.H.,  Jr.,  and  Kvenvolden,  K.,  1980,  Diapir-like 
ridges  and  possible  hydrocarbon  occurrence,  northern  California 
continental  margin:  American  Association  of  Petroleum  Geolo- 
gists Bulletin,  v.  64,  p.  706. 


Field,  M.E.,  Clarke,  S.H.,  Jr.,  and  White,  M.E.,  1980,  Geology  and 
geologic  hazards  of  offshore  Eel  River  basin,  northern  California 
continental  margin:  U.S.  Geological  Survey  Open-File  Report 
80-1080,  80  p. 

Field,  M.E.,  and  Edwards,  B.D.,  1979,  The  role  of  mass  movements 
in  basin  filling;  evidence  from  the  California  continental  margin: 
Geological  Society  of  America  Abstracts  with  Programs,  v.  11, 
p.  425. 

Field,  M.E.,  and  Edwards,  B.D.,  1980,  Slopes  of  the  southern  Califor- 
nia continental  borderland;  a  regime  of  moss  transport,  in  Field, 
M.W.,  Bouma,  A.H.,  Colburn,  I.P.,  Douglas,  R.G.,  and  Ingle,  J.C, 
editors.  Quaternary  depositionol  environments  of  the  Pacific 
coast:  Society  of  Economic  Paleontologists  and  Mineralogists, 
Pacific  Section,  Pacific  Coast  Paleography  Symposium,  no.  4,  p. 
180-196. 

Field,  M.E.,  and  Edwards,  B.D.,  1981,  Large  submarine  slump  off 
Eureka,  California:  American  Association  of  Petroleum  Geolo- 
gists Bulletin,  V.  65,  p.  924. 

Field,  M.E.,  Edwards,  B.D.,  and  Chezar,  H.,  1984,  Sediment  patterns 
resulting  from  liquefaction  of  a  shelf  sand  body:  Shelf  Sands 
Sandstone  Conference  University,  Calgary,  Alberta. 

Field,  M.E.,  Edwards,  B.D.,  Kenyon,  N.H.,  and  Somers,  M.L,  1984, 
Side-scan  sonar  mops  of  the  entire  southern  California  border- 
land and  adjacent  seomount  province:  Geological  Society  of 
America  Abstracts  with  Programs,  v.  16,  no.  6,  p.  508. 

Field,  M.E.,  Edwards,  B.D.,  Kenyon,  N.H.,  Somers,  M.L.,  and  Hey, 
R.N.,  1984,  Volcanic  and  depositionol  patterns  on  the  seafloor 
off  southern  California  as  seen  by  GLORIA  side-scon  sonar: 
American  Geophysical  Union,  Fall  Meeting,  Son  Francisco,  EOS, 
V.  65,  no.  45,  p.  1083. 

Field,  M.E.,  Edwards,  B.D.,  and  Gardner,  J.V.,  1984,  Side-scan  sonar 
and  photogrohic  survey  of  the  1980  earthquake-induced  seafloor 
failure  off  northern  California:  American  Geophysical  Union  Fall 
Meeting,  Son  Francisco,  EOS,  v.  65,  no.  45,  p.  851. 

Field,  M.E.,  and  Gardner,  J.V.,  1980,  Shale  diopirism  on  the  northern 
California  margin:  Geological  Society  of  America  Abstracts  with 
Programs,  v.  8,  p.  425. 

Field,  M.E.,  Gardner,  J.V.,  Jennings,  A.E.,  and  Edwards,  B.D.,  1981, 
Seafloor  failures  caused  by  the  November  8,  1980  earthquake 
off  northern  California:  U.S.  Geological  Survey  Open-File  Report 
81-393,  p.  27. 

Field,  M.E.,  Gardner,  J.V.,  Jennings,  A.E.,  and  Edwards,  B.D.,  1982, 
Earthquake  induced  sediment  failures  on  a  0.25°  slope,  Klamath 
River  delta,  California:  Geology,  v.  10,  p.  542-546. 

Field,  M.E.,  Jennings,  A.E.,  Gardner,  J.V.,  Chose,  T.E.,  Miller,  C.P., 
and  Young,  J.D.,  1981,  High  resolution  seismic  reflection  profiles 
collected  from  offshore  northern  California  after  the  November 
8,  1980  earthquake;  U.S.  Geological  Survey  Open-File  Report 
81-394. 

Field,  M.E.,  Kvenvolden,  K.A.,  and  Clarke,  S.H.,  1979,  Location  and 
hydrocarbon  content  of  a  gravity  core  from  the  offshore  Eel  River 
basin,  northern  California:  U.S.  Geological  Survey  Open-File 
Report  79-1618. 

Field,  M.E.,  and  Richmond,  W.C,  1980,  Sedimentary  and  structural 
patterns  on  the  northern  Santo  Rosa  -  Cortes  Ridge,  southern 
California:  Marine  Geology,  v.  34,  p.  79. 

Fischer,  P. J.,  1972,  Geologic  evolution  and  Quaternary  geology  of 
the  Santo  Barbara  basin,  California:  University  of  Southern  Cali- 
fornia unpublished  Doctoral  Thesis. 

Fischer,  P. J.,  1973,  Environmental  hazards  of  the  northern  Santa 
Barbara  shelf,  California:  Geological  Society  of  America  Ab- 
stracts with  Programs,  v.  5,  p.  42. 

Fischer,  P.J.,  1976,  Late  Neogene-Quoternory  tectonics  and  deposi- 
tionol environments  of  the  Santa  Barbara  basin,  California,  in 
Fritsche,  A.E.,  Terbest,  J.,  Jr.,  and  Wornhardt,  W.W.,  editors.  The 


84 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


Neogene  symposium:  Society  of  Economic  Paleontologists  ond 
Mineralogists.  Pacific  Section,  p.  33-52. 

Fischer,  P. J.,  1976,  Tectonic  clossification  of  shelves,  California  con- 
tinental borderlond:  Geological  Society  of  America  Abstracts 
with  Programs,  v.  8,  p.  866. 

Fischer,  P. J.,  and  Berry,  R.W.,  1978,  Offshore  fine  sediment  trans- 
port: Cool  Oil  Point,  southern  Californio:  Geological  Society  of 
America  Abstracts  with  Progroms,  v.   10,  p.  195. 

Fischer,  P.J.,  and  Berry,  R.W.,  and  Reed,  W.E.,  1976,  Southern 
California  bight:  sediment  chorocteriiotion  and  analysis  for  Bu- 
reau of  Land  Management  baseline  study:  U.S.  Bureau  of  Land 
Management,  Report  3,  p.  1-164. 

Fischer,  P. J.,  and  Kolpock,  R.L.,  1971,  Marine  geology  of  the  north- 
ern shelf  of  the  Santa  Barbara  basin — Holocene  faulting,  natural 
oil  seeps,  ond  sediments:  Geological  Society  of  America  Ab- 
stracts with  Programs,  v.  3,  p.  565. 

Fischer,  P. J.,  and  Lee,  C.F.,  1974,  Structural  control  of  submarine 
canyons,  southern  California:  Geological  Society  of  America  Ab- 
stracts with  Progroms,  v.  6,  p.  735-736. 

Fischer,  P. J.,  Rudat,  J.,  and  Ticken,  E.,  1979,  Recognition  of  active 
(Holocene)  faulting,  southern  California  borderland:  Geological 
Society  of  Americo  Abstrocts  with  Programs,  v.  11,  p.  78. 

Fischer,  P. J.,  and  Stevenson,  A. J.,  1973,  Natural  hydrocarbon  seeps 
along  the  northern  shelf  of  the  Santa  Barbara  basin,  California: 
American  Association  of  Petroleum  Geologists,  and  Society  of 
Economic  Paleontologists  and  Minerologists,  Pacific  Sections, 
Guidebook,  Joint  Annuol  Meeting. 

Fischer,  R.V.,  and  Charlton,  D.W„  1976,  Mid-Miocene  Blanco  For- 
mation, Santo  Cruz  Islond,  California,  In  Howell,  D.G.,  editor. 
Aspects  of  the  geologic  history  of  the  California  continental 
borderland:  American  Association  of  Petroleum  Geologists,  Po- 
cific  Section,  Miscellaneous  Publicotion  24,  p.  228-239. 

Fleischer,  P.,  1969,  Mineralogy  of  Holocene  basin  sediments,  Califor- 
nia continentol  borderland:  Geological  Society  of  Americo  Ab- 
strocts with  Programs,  v.   1,  p.  67-68. 

Fleischer,  P.,  1970,  Effect  of  late  Pleistocene  sea  level  rise  on  basin- 
sediment  mineralogy:  American  Quaternary  Association  First 
Meeting,  p.  46. 

Fleischer,  P.,  1970,  Minerology  of  hemipelogic  basin  sediments,  Cali- 
fornia continental  borderland:  University  of  Southern  California, 
Department  of  Geological  Science,  Special  Publication,  208  p. 

Fleischer,  P.,  1972,  Mineralogy  and  sedimentation  history,  Santo 
Borboro  basin,  California:  Journal  of  Sedimentory  Petrology,  v. 
42,  p.  49-58. 

Fluty,  L.,  and  Marks,  S.M.,  1981,  Catalog  of  earthquakes  along  the 
Son  Andreas  fault  system  in  central  California,  October  -  Decem- 
ber, 1977:  U.S.  Geological  Survey  Open-File  Report  81-1325,  48 

P- 
Ford,  G.A.,  and  Normork,  W.R.,   1980,  Mop  showing  o  deep-tow 

geophysicol  study  of  the  north  end  of  the  Son  Clemente  foult, 

Colifornio   borderland:   U.S.   Geological   Survey   Miscellaneous 

Field  Studies  Mop  MF-1230,  1  sheet. 
Formon,  J. A.,  1970,  Age  of  the  Catalino  Island  pluton,  California: 

Geologlcol  Society  of  America  Special  Paper  124,  p.  37-45. 
Formon,   J. A.,    Edwords,   L.N.,   and   Terpening,   J.N,,    1972,    Upper 

Miocene  volconic  rocks,  Fishermon's  Cove  oreo,  Santo  Cotolino 

Island,  California:  Geologicol  Society  of  America  Abstracts  with 

Progroms,  v.  4,  p.   159. 
Formon,  J.A.,  Hall,  K.B.,  Weaver,  D.W.,  Kennelt,  W.E.,  Redin,  T.W., 

and  Redwine,  L.E.,  1968,  Field  trip  guide  to  Santo  Roso  Island: 

American  Association  of  Petroleum  Geologists  and  Society  of 

Economic   Paleontologists   and   Mineralogists,   Pacific   Sections, 

number  3,  7  p. 
Fowler,  G.A.,  1958,  Submarine  topography  and  geology  of  Lasuen 

Seomount,  southern  Colifornio:  University  of  Southern  California 

unpublished  report  in  Morine  Geology,  1 1  p. 


Fowler,  G.A.,  1963,  Submorine  geology  of  Lasuen  Bonk:  American 
Association  of  Petroleum  Geologists  Bulletin,  v.  47,  p.  1770. 

Frame,  R.G.,  1960,  Californio  offshore  petroleum  development:  Cali- 
fornia Division  of  Oil  and  Gos,  Colifornio  Oil  Fields — Summary 
of  Operations,  v.  46,  p.  5-46. 

Friedmon,  M.E.,  Whitcomb,  J.H.,  Allen,  C.R.,  ond  Hilemon,  J.A., 
1976,  Seismicity  of  the  southern  Colifornio  region,  1  Jonuory 
1972  to  32  December  1974:  California  Institute  of  Technology, 
Division  of  Geological  and  Planetary  Sciences  Contribution 
2734,  404  p. 

Puis,  G.S.,  Friedman,  MR.,  ond  Hilemon,  J. A.,  1977,  Preliminory 
catalog  of  eorthquokes  in  southern  California,  July  1974  -  Sep- 
tember 1976:  U.S.  Geological  Survey  Open-File  Report  77-181. 

Goal,  R.A.P.,  1966,  Marine  geology  of  the  Sonto  Cotolino  bosin, 
California:  Pacific  Science  Congress  Proceedings,  1 1th  Congress, 
p.  288. 

Gaol,  R.A.P.,  1966,  Morine  geology  of  the  Sonto  Cotolino  basin 
oreo,  Colifornio:  University  of  Soutfiern  California  unpublished 
Doctorol  Thesis. 

Gamble,  J.H.,  1957,  Geology  of  the  Point  Mugu  ond  Comorillo 
quadrangles,  Ventura  County,  Colifornio;  University  of  Califor- 
nia, Los  Angeles,  unpublished  Doctoral  Thesis. 

Gordett,  P.H.,  1971,  Petroleum  potential  of  Los  Angeles  basin,  Cali- 
fornia, in  Cram,  I.H.,  editor.  Future  petroleum  provinces  of  the 
United  States — their  geology  and  potential:  Americon  Associa- 
tion of  Petroleum  Geologists  Memoir  15,  v.  1,  p.  298-308. 

Gardner,  J.V.,  Barron,  J.A.,  Dean,  W.E.,  Poore,  R.Z.,  Quintero,  P.J., 
Stone,  S.M.,  and  Wilson,  C.R.,  1983,  Quontitotive  microfossil, 
sedimentologic,  and  geochemicol  data  on  core  L13-81-6138  ond 
surface  samples  from  the  continentol  shelf  and  slope  of  northern 
California:  U.S.  Geological  Survey  Open-File  Report  84-369,  1 18 

P- 

Gardner,  J.V.,  Deon,  W.E.,  Huessen,  L.E.,  Klise,  D.H.,  Poore,  R.Z., 
Quintero,  P. J.,  and  Stone,  S.M.,  1983,  Quontitotive  microfossil, 
sedimentologic,  ond  geochemicol  doto  on  cores  V1-80-P3  ond 
V1-80-G1,  ond  V1-80-P8  from  the  continentol  slope  of  northern 
Colifornio:  U.S.  Geologicol  Survey  Open-File  Report  83-83,  p. 
51. 

Gordner,  J.V.,  and  Klise,  D.H.,  1983,  Minerologicol  and  sedimento- 
logical  doto  collected  on  the  shelf  ond  upper  slope  adjacent  to 
the  Russian  River,  northern  Colifornio:  U.S.  Geological  Survey 
Open-File  Report  83-517,  35  p. 

Gordner,  J.V.,  McCulloch,  D.S.,  Eittreim,  S.L.,  and  Mosson,  D.G., 
1984,  Long-range  side-scon  sonor  studies  of  the  centrol  Colifor- 
nio EEZ:  Geological  Society  of  Americo  Abstracts  with  Programs. 
V.  16.  no.  6.  p.  515. 

Garfunkel.  A.,  1973.  History  of  the  Son  Andreas  fault  as  o  plate 
boundary:  Geological  Society  of  America  Bulletin,  v.  84,  p.  2035- 
2042. 

Garrison,  L.E.,  and  Tokohosi,  K.J.,  1950,  Bottom  samples  off  the 
coast  of  southern  California:  Scripps  Institute  of  Oceonography, 
Submorine  Geology  Report,  6  p. 

Goskell,  T.F.,  1965,  The  prospects  for  offshore  oil:  New  Scientist,  v. 
27,  p.  265-266. 

Gowthrop,  W.H.,  1975,  Seismicity  of  the  centrol  Colifornio  coostol 
region:  U.S.  Geological  Survey  Open-File  Report  75-134. 

Gowthrop.  W.H..  1977.  Seismicity  and  tectonics  of  the  central  Coli- 
fornio coastal  region:  University  of  Colorado  unpublished 
Moster's  Thesis.  76  p. 

Gowthrop.  W.H,.  1978,  Seismicity  ond  tectonics  of  the  centrol  Cali- 
fornia coastal  region,  in  Silver.  E.A..  and  Normork.  W.R..  editors. 
San  Gregorio-Hosgri  fault  zone.  California:  California  Division  of 
Mines  ond  Geology  Special  Report  137,  p.  45-56. 

Gowthrop.  W.H..  1978.  The  1927  Lompoc.  Californio,  eorthquoke: 
Seismologicol  Society  of  Americo  Bulletin,  v.  68.  p.  1705-1716. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


85 


Gawthrop,  W.H.  and  Engdahl,  E.R.,  1975,  The  1927  Lompoc  earth- 
quake and  the  1969  San  Luis  Bank  earthquake  sequence,  a 
comparative  study:  American  Geophysical  Union  Transactions,  v. 
56,  p.  1028. 

Gerin,  M.,  1977,  Bathymetric  map  of  Pacific  coast:  Crescent  City  to 
Davenport,  California:  U.S.  Geological  Survey  Open-File  Report 
77-208. 

Gerin,  M.,  and  Schumacher,  G.M.,  1977,  Bathymetric  map  of  Pacific 
coast:  Monterey  Boy  to  Gulf  of  Santa  Catalino:  U.S.  Geological 
Survey  Open-File  Report  77-247,  1  p. 

Gerin,  M.,  and  Shryock,  P.,  1977,  Bathymetric  map  of  Pacific  Ocean 
southwest  of  Point  Santa  Cruz,  California:  U.S.  Geological  Sur- 
vey Open-File  Report  77-515. 

Gibson,  J.M.,  and  Prensky,  S.,  1972,  Poleoclimatic  and  faunal 
events  recorded  in  Holocene/late  Pleistocene  marine  sediments 
of  the  San  Clemente  basin,  California  borderland  and  their  possi- 
ble tectonic  significance:  Geological  Society  of  America  Ab- 
stracts with  Programs,  v.  4,  p.  161-162. 

Gieser,  H.S.,  1927,  Mining  and  milling  on  Santa  Cotolina  Island: 
Engineering  and  Mining  Journal,  v.  124,  p.  245-247. 

Gilluly,  J.,  and  Grant,  U.S.,  IV,  1949,  Subsidence  in  the  Long  Beach 
harbor  area,  California:  Geological  Society  of  America  Bulletin, 
v.  60,  p.  461-530. 

Goodwin,  D.G.,  1952,  Some  decapod  Crustacea  dredged  off  the 
coast  of  central  California:  Proceedings  of  the  California  Acade- 
my of  Sciences,  Fourth  Series,  v.  27,  p.  393-397. 

Goodyear,  W.A.,  1890,  San  Diego  County,  Santa  Cruz  Island:  Cali- 
fornia State  Mineralogist,  9th  Annual  Report,  p.  139-170. 

Gorsline,  D.S.,  1958,  Marine  geology  of  Son  Pedro  and  Santo 
Monica  basins  and  vicinity,  California:  University  of  Southern 
California  unpublished  Doctoral  Thesis. 

Gorsline,  D.S.,  1968,  Marine  geology  of  the  California  continental 
borderland:  University  of  Southern  California,  Department  of 
Geological  Sciences  Report  USC-GEOL  68-1,  92  p. 

Gorsline,  D.S.,  1970,  Report  of  a  reconnaissance  survey  of  th^ 
hydrographic  characteristics  of  the  Hueneme-Mugu  shelf  to 
evaluate  ground-water  leakage  from  submarine  exposures  of 
coastal  aquifers,  June-July,  1970:  University  of  Southern  Califor- 
nia, Department  of  Geological  Sciences  Report  USC-GEOL  70-6, 
21  p. 

Gorsline,  D.S.,  1971,  Sedimentation  in  late  Pleistocene  and  Holo- 
cene  time  in  California  continental  borderland  basins:  National 
Coastal  Shallow  Water  Resources,  Conference,  Abstract  Number 
2,  p.  89. 

Gorsline,  D.S.,  1971,  Wisconsin  sedimentation  in  Tanner  basin,  Cali- 
fornia continental  borderland;  a  record  of  Pleistocene  climate: 
Geological  Society  of  America  Abstracts  with  Programs,  v.  3,  p. 
126. 

Gorsline,  D.S.,  1976,  Patterns  of  California  continental  borderland 
sedimentation  derived  from  late  Pleistocene  and  Holocene  stud- 
ies: American  Association  of  Petroleum  Geologists  Bulletin,  v.  60, 
p.  2181. 

Gorsline,  D.S.,  1978,  Anatomy  of  margin  basins:  Journal  of  Sedi- 
mentary Petrology,  v.  48,  p.  1055-1068. 

Gorsline,  D.S.,  1980,  Depositional  patterns  of  hemipelogic  sedi- 
ments in  borderland  basins  on  on  active  margin,  in  Field,  M.E., 
Bouma,  A.H.,  Coldburn,  I. P.,  Douglas,  R.G.,  and  Ingle,  J.C,  edi- 
tors. Quaternary  depositional  environments  of  the  Pacific  coast: 
Society  of  Economic  Paleontologists  and  Mineralogists,  Los  An- 
geles, p.  185-200. 

Gorsline,  D.S.,  1980,  Sedimentologic  history  and  characteristics  of 
continental  margin  basins,  California  borderlond:  American  As- 
sociation of  Petroleum  Geologists  Bulletin,  v.  64,  p.  442-443. 

Gorsline,  D.S.,  1981,  Fine  sediment  transport  and  deposition  in 
active  basins,  in  Douglas,  R.G.,  Colburn,  I. P.,  and  Gorsline,  D.S., 
editors,  Depositional  systems  of  active  continental  morgin  basins; 


Short  course  notes:  Society  of  Economic  Paleontologists  and 
Mineralogists,  Pacific  Section,  Los  Angeles,  p.  39-60. 

Gorsline,  D.S.,  and  Barnes,  P.W.,  1970,  Evidence  for  Holocene  cli- 
matic changes  from  Tanner  and  Santa  Cruz  basins,  California 
continentol  borderland:  American  Quaternary  Association's  first 
meeting,  p.  54. 

Gorsline,  D.S.,  and  Barnes,  P.W.,  1972,  Carbonate  variations  as 
climatic  indicators  in  contemporary  California  flysch  basins:  Pro- 
ceedings, 24th  International  Geological  Congress,  Section  6, 
Montreal,  Abstracts,  p.  186. 

Gorsline,  D.S.,  Barnes,  P.W.,  Beer,  R.M.,  and  Honer,  B.E.,  1967, 
Studies  of  submarine  canyons  and  fans  off  southern  California: 
University  of  Southern  California,  Department  of  Geological 
Science  Report  USC-GEOL  76-3,  27  p. 

Gorsline,  D.S.,  Brenninkmeyer,  B.M.,  Meyer,  W.S.,  Ploessel,  M.R., 
Shiller,  G.I.,  and  Vonder  Hoar,  S.P.,  1971,  General  characteris- 
tics of  nearshore  sediments  from  El  Copiton  to  Ventura,  Califor- 
nia, 1967-70,  in  Kolpack,  R.L.,  editor.  Biological  and 
oceanogrophicol  survey  of  the  Santo  Barbara  Channel  oil  spill, 
1969-70:  University  of  Southern  California,  Allan  Hancock  Foun- 
dation, V.  2,  p.  296-317. 

Gorsline,  D.S.,  Drake,  D.E.,  and  Barnes,  P.W.,  1968,  Holocene  sedi- 
mentation in  Tanner  basin,  California  continental  borderland: 
Geological  Society  of  America  Bulletin,  v.  79,  p.  659-674. 

Gorsline,  D.S.,  and  Emery,  K.O.,  1959,  Turbidity-current  deposits  in 
San  Pedro  and  Santa  Monica  basins  off  southern  California: 
Geological  Society  of  America  Bulletin,  v.  70,  p.  279-290. 

Gorsline,  D.S.,  and  Grant,  D.J.,  1972,  Sediment  textural  patterns  on 
San  Pedro  shelf,  California  ( 1951-1971 ),  m  Swift,  D.J. P.,  Duone, 
D.B.,  and  Pilkey,  O.H., ,  editors.  Shelf  sediment  transport:  Dowd- 
en  Hutchinson,  and  Ross,  Inc.,  Stroudsburg,  Pennsylvania,  p. 
575-600. 

Gorsline,  D.S.,  Grant,  D.J.,  and  Booth,  J.S.,  1971,  Heavy  mineral 
content  of  river,  beach  and  nearshore  sediments,  southern  Cali- 
fornia: University  of  Southern  California,  Department  of  Geolog- 
ical Sciences  Report,  USC-GEOL  71-5,  76  p. 

Gorsline,  D.S.,  Poo,  G.A.,  Prensky,  S.E.,  and  Mulhern,  M.,  1976, 
High-resolution  studies  of  poleoclimatic  and  paleoceonographic 
history  in  California  continental  borderland  basin  sediments: 
American  Association  of  Petroleum  Geologists  Bulletin,  v.  60,  p. 
675. 

Gorsline,  D.S.,  and  Prensky,  S.E.,  1975,  Poleoclimatic  inferences  for 
late  Pleistocene  and  Holocene  from  California  continental  bor- 
derland basin  sediments,  in  Subbate,  R.P.,  and  Creswell,  M.M., 
editors.  Quaternary  Studies:  Royal  Society  of  New  Zealand, 
Wellington,  p.  147-154. 

Grady,  J.R.,  1955,  Submarine  geology  of  Santo  Barbara  Island  and 
vicinity:  University  of  Southern  California  unpublished  Master's 
Thesis. 

Graham,  S.A.,  1976,  Tertiary  sedimentary  tectonics  of  the  central 
Salinian  block  of  California:  Stanford  University,  California  un- 
published Doctoral  Thesis,  213  p. 

Graham,  S.A.,  and  Dickinson,  W.R.,  1978,  Evidence  for  1 15  kilome- 
ters of  right  slip  of  the  San  Gregorio-Hosgri  fault  trend:  Science, 
v.  199,  p.  178-181. 

Grohom,  S.A.,  McCloy,  C,  Hitzmon,  M.,  Word,  R.,  and  Turner,  R., 
1984,  Basin  evolution  during  change  from  convergent  to  trans- 
form continental  margin  in  central  California:  American  Associa- 
tion of  Petroleum  Geologists  Bulletin,  v.  68,  p.  233-249. 

Gram,  R.,  1974,  The  marine  geology  of  the  recent  sediments  of 
central  Son  Francisco  Boy:  Geological  Society  of  America  Ab- 
stracts with  Programs,  v.  6,  p.   182. 

Grant,  D.J.,  1972,  Sediment  textural  patterns  on  the  Son  Pedro 
shelf,  California:  University  of  Southern  California  unpublished 
Master's  Thesis. 


86 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


Grant,  U.S.,  IV,  and  Sheppard,  W.E.,  1939,  Some  recent  changes 
of  elevotion  in  the  Los  Angeles  basin  of  southern  California,  and 
their  possible  significonce:  Seismological  Society  of  America  Bul- 
letin, V.  29,  p.  299-326. 

Gray,  C.F.,  Jr.,  Kennedy,  M.P.,  and  Morton,  P.K.,  1971,  Petroleum 
potential  of  southern  coastal  ond  mountain  area,  California,  in 
Future  petroleum  provinces  in  the  United  States — their  geology 
and  potential:  American  Association  of  Petroleum  Geologists 
Memoir  15,  p.  372-383. 

Green,  P.,  1976,  E.P.A.'s  view  of  projected  oil  drilling  on  the  conti- 
nental shelf:  Seo  Technology,  Compass  Publicatins,  Arlington, 
Virginia,  v.   17,  p.  11-13. 

Greene,  H.G.,  1970,  Geology  of  southern  Montery  Boy  and  its 
relationship  to  the  ground  water  basin  and  salt  water  intrusion: 
U.S.  Geological  Survey  Open-File  Report,  50  p. 

Greene,  H.G.,  1972,  Geology  and  present  day  faulting  of  the  Mon- 
terey Bay  region:  American  Institute  of  Professional  Geologists 
Convention,  Program  Abstracts. 

Greene,  H.G.,  1976,  Late  Cenozoic  geology  of  the  Ventura  basin, 
California,  in  Howell,  D.G.,  editor,  Aspects  of  the  geologic  his- 
tory of  the  California  continental  borderlond:  American  Associa- 
tion of  Petroleum  Geologists,  Pacific  Section,  Miscellaneous 
Publication  24,  p.  499-540. 

Greene,  H.G.,  1977,  Geology  of  the  Monterey  Bay  region:  U.S. 
Geological  Survey  Open-File  Report  77-718,  p.  340. 

Greene,  H.G.,  1977,  Monterey  submarine  canyon:  California  Geol- 
ogy, V.  30,  p.  112-113. 

Greene,  H.G.,  1977,  Slivering  of  the  Solinion  block  along  the  Palo 
Colorado  -  Son  Gregorio  and  associated  fault  zones:  Geological 
Society  of  America  Abstracts  with  Programs,  Cordilleran  Section, 
73rd  Annual  Meeting,  Sacramento,  California,  v.  9,  no.  4,  p.  425. 

Greene,  H.G.,  1978,  Geology  of  the  Monterey  Boy  region:  U.S. 
Geological  Survey  Professional  Paper  1100,  p.   151. 

Greene,  H.G.,  1980,  Quaternary  tectonics,  offshore  Los  Angeles  - 
San  Diego  area,  in  Turner,  M.L.,  editor.  Summaries  of  Technical 
Reports,  V.  9,  p.  11-12:  U.S.  Geological  Survey,  Office  of  Earth- 
quake Studies  Open-File  Report  80-6. 

Greene,  H.G.,  1980,  Submarine  canyons  as  on  indicator  of  nappe 
development  along  the  transform  boundary  of  California,  in  26th 
International  Geological  Congress  Abstracts,  v.  2,  Poris,  France, 
p.  479. 

Greene,  H.G.,  Bailey,  K.A.,  Clarke,  S.H.,  Ziony,  J. I.,  and  Kennedy, 
M.P.,  1979,  Implications  of  fault  patterns  of  the  inner  California 
continental  borderland  between  Son  Pedro  and  San  Diego,  in 
Abbott,  P.L.,  and  Elliott,  W.J.,  editors.  Earthquakes  and  other 
perils.  Son  Diego  region:  Son  Diego  Associotion  of  Geologists 
Publication,  p.  21-27. 

Greene,  H.G.,  and  Clark,  J.C,  1979,  Neogene  poleogeogrophy  of 
the  Monterey  Boy  area,  California,  in  Cole,  M.R.,  Terbest,  H., 
and  Aremntrout,  J.,  editors,  Cenozoic  poleogeogrophy  of  the 
western  United  States:  Pacific  Society  of  Economic  Paleontolo- 
gists and  Mineralogists,  Pacific  Coast  Poleogeogrophy  Sympo- 
sium 3,  p.  277-296. 

Greene,  H.G.,  Clarke,  S.H.,  and  Seekins,  B.S.,  1980,  Offshore  seis- 
mic reflection  profiles  in  the  vicinity  of  the  Cristionitos  fault,  San 
Onofre,  Californio:  U.S.  Geological  Survey  Open-File  Report 
80-945,  7  p. 

Greene,  H.G.,  Clarke,  S.H.,  Jr.,  and  Field,  M.E.,  1979,  Environmental 
geology  of  the  southern  California  borderland:  U.S.  Geological 
Survey  Professional  Paper  1150,  p.  147 

Greene,  H.G.,  Clarke,  S.H.,  Jr.,  and  Field,  M.E.,  1980,  Southern 
California  borderland,  environmental  geology:  U.S.  Geological 
Survey  Professional  Paper  1175,  p.   100 

Greene,  H.G.,  Clarke,  S.H.,  Jr.,  Field,  M.E.,  Linker,  F.I.,  and  Wagner, 
H.C.,  1975,  Preliminary  report  on  the  environmenfol  geology  of 


selected  areas  of  the  southern  California  continental  borderland: 
U.S.  Geological  Survey  Open-File  Report  75-596,  69  p.  ,  16 
mapsheets. 

Greene,  H.G.,  and  Conrey,  B.L.,  1966,  Seismic  investigation  of  Eel 
submorine  canyon,  Flumboldt  County,  Colifornio:  American  As- 
sociation of  Petroleum  Geologists  Bulletin,  v.  50,  p.  648. 

Greene,  H.G.,  and  Kennedy,  M.P.,  1980,  Review  of  offshore  seismic 
reflector  profiles  in  the  vicinity  of  the  Cristionitos  fault,  Son 
Onofre,  California;  safety  evaluation  report  (geology  and  seis- 
micity)  related  to  the  operation  of  Son  Onofre  Nuclear  generat- 
ing station.  Units  2  and  3,  p.  F3-F23,  Nuclear  Regulatory 
Commission,  Office  of  Nuclear  Reaction  Regulation,  Washing- 
ton, D.C. 

Greene,  H.G.,  and  Kennedy,  M.P.,  1980,  Addendum  to  review  of 
seismic  reflection  profiles  in  the  vicinity  of  the  Cristionitos  fault, 
San  Onofre,  California:  U.S.  Geological  Survey  administrative 
report  to  the  U.S.  Nuclear  Regulatory  Commission,  5  p.,  2  plates. 

Greene,  H.G.,  Kennedy,  M.P.,  and  McCarthy,  R.,  1981,  New  marine 
geology  mop  series,  a  tool  for  California  coastal  planners,  in 
Edge,  B.G.,  editor,  Coastal  Zone  80  Symposium  Conference,  v. 
4,  p.  2792-2796. 

Greene,  H.G.,  Lee,  W.H.K.,  McCulloch,  D.S.,  and  Brobb,  E.E.,  1973, 
Faults  and  earthquakes  in  the  Monterey  Boy  region,  California: 
U.S.  Geological  Survey  Miscelloneous  Field  Studies  Mop  MF- 
518,  14  p. 

Greene,  H.G.,  McCulloch,  D.S.,  ond  Lee,  W.H.K.,  1973,  Relation- 
ships of  the  faults  in  Monterey  Bay  region  to  the  San  Andreas 
fault,  in  Program  for  the  conference  on  the  tectonic  problems  of 
the  Son  Andreas  fault  system:  Stonford  University,  p.  21. 

Greene,  H.G.,  Moore,  J.E.,  and  Golt,  J. A.,  1983,  The  physical  envi- 
ronment and  its  effect  on  offshore  oil  and  gas  development,  in 
Gilbert,  J.T.E.,  Technical  environmental  guidelines  for  offshore  oil 
and  gas  development:  PennWell,  Tulso,  p.  15-48. 

Greene,  H.G.,  Silver,  E.A.,  and  von  Huene,  R.,  1975,  Seismic  reflec- 
tion profiles  USNS  BARTLETT,  November,  1972  cruise,  offshore 
central  and  southern  California:  U.S.  Geological  Survey  Open- 
File  Report  75-121,  75  p.,  4-trock  charts  ot  1:250,000  scale. 

Greene,  H.G.,  Wolf,  S.C,  and  Blom,  K.G.,  1972,  Late  Cenozoic 
structure  and  sedimentary  history  of  southeastern  Sonto  Barbara 
Channel  region,  Colifornio:  Geological  Society  of  America  Ab- 
stracts with  Progroms,  v.  4,  p.  164. 

Greene,  H.G.,  Wolf,  S.C,  and  Blom,  K.G.,  1974,  The  morine  geol- 
ogy of  the  eastern  Sonto  Borboro  Channel  with  porticuor  empha- 
sis on  the  ground  water  basins  offshore  from  the  Oxnord  plain, 
southern  Colifornio:  U.S.  Geologicol  Survey  Open-File  Report. 

Greene,  H.G.,  Wolf,  S.C,  and  Blom,  K.G.,  1978,  The  marine  geol- 
ogy of  the  neorshore  Ventura  basin  and  its  relationship  to  the 
ground  water  basins  of  Oxnord  plain:  U.S.  Geological  Survey 
Open-File  Report  78-30,  5  p. 

Griggs,  G.B.,  and  Hein,  J.R.,  1979,  Sources,  magnitudes,  and  disper- 
sal of  fine-grained  sediment  off  central  and  northern  Colifornio: 
Geological  Society  of  America  Abstracts  with  Progroms,  v.  11, 
p.  80-81. 

Griggs,  G.B.,  and  Hein,  J.R.,  1980,  Sources,  dispersal,  ond  clay 
mineral  composition  of  finegrained  sediment  off  central  and 
northern  California:  University  of  Chicago  Press,  Chicago,  Illinois, 
V.  88,  p.  541-566,  illustrations  (tobies  and  sketch  mops  includ- 
ed!. 

Grim,  R.E.,  Dietz,  R.S.,  and  Bradley,  W.F.,  1949,  Cloy  mineral  com- 
position of  some  sediments  from  the  Pacific  Ocean  off  the  Cali- 
fornia coast  and  the  Gulf  of  California:  Geological  Society  of 
America  Bulletin,  v.  60,  p.   1785-1808. 

Griscom,  A.,  1980,  Aeromognetic  interprelotion  of  the  Mendocino 
triple  junction,  in  Streitz,  R.,  ond  Sherburne,  R.,  editors.  Studies 
of  the  San  Andreas  fault  in  northern  California:  Californio  Divi- 
sion of  Mines  and  Geology,  Special  Report  140,  p.  121-130. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


87 


Guttenberg,  B.,  1943,  Earthquakes  and  structure  in  southern  Califor- 
nia: Geological  Society  of  America  Bulletin,  v.  54,  p.  499-526. 

Guttenberg,  B.,  1951,  Revised  travel  times  in  southern  California: 
Seismological  Society  of  America  Bulletin,  v.  41,  p.  143-163. 

Guttenberg,  B.,  Richter,  C.F.,  and  Wood,  H.O.,  1932,  The  earth- 
quake in  Santa  Monica  Bay,  California,  on  August  30,  1930: 
Seismological  Society  of  America  Bulletin,  v.  22,  p.  138-154. 

Hafner,  W.,  1940,  The  seismic  velocity  distribution  in  the  Tertiary 
basins  of  California:  Seismological  Society  of  America  Bulletin, 
V.  30,  p.  309-326. 

Hall,  C.A.,  1975,  Son  Simeon  -  Hosgri  fault  system,  coastal  Califor- 
nia— economic  ond  environmental  implications:  Science,  v.  190, 
p.  1291-1294. 

Hall,  C.A.,  1976,  Geologic  map  of  the  Son  Simeon  -  Piedras  Blancas 
region,  San  Luis  Obispo  County,  California:  U.S.  Geological 
Survey  Map  MF-784. 

Hall,  C.A.,  1978,  Origin  and  development  of  the  Lompoc-Santa 
Mario  pull-aport  basin  and  its  relation  to  the  San  Simeon-Hosgri 
strike-slip  fault,  western  California,  in  Silver,  E.A.,  and  Normark, 
W.R.,  editors,  San  Gregorio-Hosgri  fault  zone,  California:  Cali- 
fornia Division  of  Mines  and  Geology  Special  Report  137,  p. 
25-32. 

Hall,  K.B,  and  Curron,  J.F.,  1969,  Summary  on  recent  developments, 
Santa  Barbara,  California:  American  Association  of  Petroleum 
Geologists  Bulletin,  v.  53,  p.  460. 

Hall,  K.B,  and  Curron,  J.F.,  1972,  Geology  and  future  petroleum 
potential,  Ventura  basin,  California,  in  Pacific  coast  geology, 
basis  for  new  exploration:  American  Association  of  Petroleum 
Geologists  and  Society  of  Exploration  Geophysicists,  Pacific 
Sections,  Technical  Program  Preprints,  17  p. 

Hall,  R.W.,  and  Ensiminger,  H.R.,  editors,  1979,  Potential  geologic 
hazards  and  constraints  for  blocks  in  proposed  mid-Atlantic  OCS 
oil  and  gas  lease  sale  49;  U.S.  Geological  Survey  Open-File 
Report  79-264,  176  p.,  12  figures,  1  plate. 

Hamilton,  E.L.,  1963,  Sediment  sound  velocity  measurements  mode 
in  situ  from  bothyscaph  TRIESTE:  Journal  of  Geophysical  Re- 
search, V.  68,  p.  5991-5998. 

Hamilton,  E.L.,  1964,  Consolidation  characteristics  and  related  prop- 
erties of  sediments  from  experimental  Mohole  (Guadalupe  site) : 
Journal  of  Geophysical  Research,  v.  69,  p.  4257-4269. 

Hamilton,  E.L.,  Shumway,  G.,  Menard,  H.W.,  and  Shipek,  C.J., 
1956,  Acoustic  and  other  physical  properties  of  shallow-water 
sediments  off  Son  Diego:  The  Journal  of  the  Acoustical  Society 
of  America,  v.  28,  p.  1-15. 

Hamilton,  N.,  and  Rees,  A. I.,  1970,  Magnetic  fabric  of  sediments 
from  the  shelf  of  La  Jollo:  Marine  Geology,  v.  9,  p.  M6-M11. 

Hamilton,  R.M.,  Yerkes,  R.F.,  Brown,  R.D.,  Jr.,  Burford,  R.O.,  and 
DeNoyer,  J.M.,  1969,  Seismicity  and  associated  effects,  Santa 
Barbara  region:  U.S.  Geological  Survey  Professional  Paper  679- 
D,  p.  47-68. 

Hamilton,  W.,  1961,  Origin  of  the  Gulf  of  California:  Geological 
Society  of  America  Bulletin,  v.  72,  p.  1307-1318. 

Hamilton,  W.,  1969,  Mesozoic  California  and  the  underflow  of  Pa- 
cific mantle:  Geological  Society  of  America  Bulletin,  v.  81,  p. 
3513-3535. 

Hamilton,  W.,  1978,  Mesozoic  tectonics  of  the  western  United 
States,  in  Howell,  D.G.,  and  McDougall,  K.A.,  editors,  Mesozoic 
paleogeography  of  the  western  United  States:  Society  of  Eco- 
nomic Paleontologist  and  Mineralogists,  Pacific  Coast  Paleo- 
geography Symposium  2,  p.  33-71. 

Hamilton,  W.,  and  Myers,  W.B.,  1966,  Cenozoic  tectonics  of  the 
western  United  States:  Reviews  of  Geophysics,  v.  4,  p.  509-549. 

Hampton,  M.A.,  and  Boumo,  A.H.,  1977,  Slope  instability  near  the 
shelf  break,  western  Gulf  of  Alaska:  Marine  Geotechnology,  v. 
2,  p.  309-322. 


Hampton,  M.A.,  Karl,  H.A.,  and  Kenyon,  N.H.,  1984,  Sonogroph 
mosaic  of  the  Oregon-Washington  EEZ:  American  Geophysical 
Union  Fall  Meeting,  Son  Francisco,  EOS,  v.  65,  no.  45,  p.  1083. 

Hampton,  M.A.,  Karl,  H.A.,  and  Kenyon,  N.H.,  1984,  Geomorphic 
features  of  the  Oregon-Washington  EEZ:  Geological  Society  of 
America  Abstracts  with  Programs,  v.   16,  no.  6,  p.  529. 

Hand,  B.M.,  1962,  Marine  geology  of  the  north  end  of  San  Diego 
trough:  University  of  Southern  California  unpublished  Master's 
Thesis. 

Hand,  B.M.,  and  Emery,  K.O.,  1964,  Turbidites  and  topography  of 
north  end  of  Son  Diego  trough:  Journal  of  Geology,  v.  72,  p. 
526-541. 

Handlin,  J.W.,  1951,  The  source,  transportation,  and  deposition  of 
beach  sediment  in  southern  California:  U.S.  Army,  Corps  of  Engi- 
neers, Beach  Erosion  Board,  Technical  Memorandum  22,  113  p. 

Honer,  B.E.,  1969,  Geomorphology  and  sedimentary  characteristics 
of  Redondo  submarine  fan,  southern  California:  University  of 
Southern  California  unpublished  Master's  Thesis. 

Honer,  B.E.,  1971,  Morphology  and  sediments  of  Redondo  subma- 
rine fan,  southern  California:  Geological  Society  of  America 
Bulletin,  V.  82,  2413-2432. 

Honer,  B.E.,  1979,  Sea  gullies  and  development  of  linear  con- 
glomeratic units:  American  Association  of  Petroleum  Geologists 
Bulletin,  V.  63,  p.  462. 

Honer,  B.E.,  and  Gorsline,  D.S.,  1978,  Processes  and  morphology  of 
continental  slope  between  Santa  Monica  and  Dume  submarine 
canyons,  southern  California:  Marine  Geology,  v.  28,  p.  77-87. 

Hanno,  G.D.,  1952,  Geology  of  the  continental  slope  off  central 
California:  Proceedings  of  the  California  Academy  of  Sciences, 
Fourth  Series,  v.  27,  p.  325-358. 

Harding,  T.P.,  1973,  Newport-lnglewood  trend,  California — on  ex- 
ample of  wrenching  style  of  deformation:  American  Association 
of  Petroleum  Geologists  Bulletin,  v.  57,  p.  97-116. 

Harmon,  R.A.,  1964,  Distribution  of  foraminifero  in  the  Santa  Bar- 
bara basin,  California:  Micropaleontology,  v.  10,  p.  81-96. 

Harris,  L.M.,  and  llfrey,  W.T.,  1969,  Drilling  in  1,300  feet  of  water — 
Santo  Barbara  Channel,  California:  Offshore  Technology  Con- 
ference, May  1969,  Paper  OTC  1018,  v.  1,  p.  167-182. 

Harrison,  J.C,  1960,  Gravity  measurements  in  the  northern  continen- 
tal borderland  area  off  southern  California,  interim  report:  Insti- 
tute of  Geophysics  and  Planetary  Physics,  University  of 
California,  Los  Angeles,  42  p. 

Harrison,  J.C,  1960,  Gravity  measurements  in  the  southern  conti- 
nental borderland  west  of  Bojo  California,  interim  report:  Insti- 
tute of  Geophysics  and  Planetery  Physics,  University  of 
California,  Los  Angeles,  65  p. 

Harrison,  J.C,  Von  Heune,  R.E.,  and  Corbato,  C.E.,  1965,  A  gravity 
map  of  the  continental  borderland  of  southern  California:  Ameri- 
can Geophysical  Union  Transactions,  v.  46. 

Harrison,  J.C,  Von  Heune,  R.E.,  and  Corbato,  C.E.,  1966,  Bouguer 
gravity  anomalies  and  magnetic  anomalies  off  the  coast  of  south- 
ern California:  Journal  of  Geophysical  Research,  v.  71,  p.  4921- 
4941. 

Hawkins,  J.W.,  and  Allison,  E.C,  1970,  Volcanic  petrology  and 
paleontology  of  Northeast  Bonk,  southern  California  borderland: 
Geological  Society  of  America  Abstracts  with  Programs,  v.  2,  p. 
99-100. 

Hawkins,  J.W.,  Allison,  E.C,  and  MocDougoll,  D.,  1971,  Volcanic 
petrology  and  geologic  history  of  Northeast  Bonk,  southern  Cali- 
fornia borderland:  Geological  Society  of  America  Bulletin,  v.  82, 
p.  219-228. 

Hawkins,  J.W.,  and  Divis,  A.F.,  1975,  Petrology  and  geochemistry 
of  mid-Miocene  volcanism  on  Son  Clemente  and  Santo  Cotolina 
Islands  and  adjacent  areas  of  the  southern  California  borderland: 
Geological  Society  of  America  Abstracts  with  Programs,  v.  7,  p. 
323-324. 


88 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


Hawkins,  J.W.,  ond  Hawkins,  D.L.,  1977,  Petrology,  geochemistry 
and  evolution  of  mid-Miocene  volcanic  rocks  of  San  Clemente 
Island,  southern  Colifornia  borderland:  Geological  Society  of 
America  Abstracts  with  Progroms,  v.  9,  p.  432. 

Hazenbush,  G.C.,  and  Allen,  D.R.,  1958,  Huntington  Beach  oil  field: 
California  Oil  Fields,  v.  44,  p.  13-25. 

Healy,  J.H.,  1963,  Crustal  structure  along  the  coast  of  California 
from  seismic-refraction  measurements:  Journol  of  Geophysical 
Research,  v.  68,  p.  5777-5787. 

Hedberg,  H.D.,  Moody,  J.D.,  and  Hedberg,  R.M.,  1979,  Petroleum 
prospects  of  the  deep  offshore:  Americon  Association  of  Petro- 
leum Geologists  Bulletin,  v.  63,  p.  286-300  (tables  and  sketch 
maps  included) . 

Heezen,  B.C.,  and  Drake,  C.L.,  1964,  Grand  Bonks  slump;  American 
Association  of  Petroleum  Geologists  Bulletin,  v.  48,  no.  2,  p. 
221-225. 

Hein,  F.J.,  1980,  Sedimentologicol  and  geotechnicol  aspects  of  fine- 
grained moss-flow  deposits,  Colifornia  borderland  basins:  Geo- 
logic Association  Canada  Annual  Management,  Halifax,  Nova 
Scotia,  p.  46. 

Hein,  F.J.,  ond  Gorsline,  D.S.,  1985,  Geotechnicol  aspects  of  fine- 
grained moss  flow  deposits;  California  continental  borderland: 
Geo-Morine  Letters,  v.  1,  p.  1-5. 

Hein,  F.J.,  and  Thornton,  S.E.,  1979,  Fine-grained  mass-flow  depos- 
its in  slope  and  slope  apron  setting;  examples  from  the  California 
borderland:  Geological  Society  of  America  Abstracts  with  Pro- 
groms, V.  11,  p.  441-442. 

Hein,  J.R.,  1973,  Deep-sea  sediment  source  areas;  implications  of 
vorioble  rates  of  movement  between  California  and  the  Pacific 
plate:  Nature,  c.  241,  no.  5384,  p.  40-41. 

Hein,  J.R.,  1973,  Increasing  rote  of  movement  with  time  between 
California  and  the  Pacific  plate,  from  Delgada  submarine  fan 
source  areas;  Journal  of  Geophysical  Research,  v.  78,  p.  7752- 
7762. 

Hein,  J.R.,  Allwardt,  A.O.,  and  Griggs,  G.B.,  1974,  The  occurrence 
of  glouconite  in  Monterey  Boy,  California,  diversity,  origins,  and 
sedimentary  environment:  Journal  of  Sedimentary  Petrology,  v. 
44,  p.  562-571. 

Heintz,  L.O.,  1966,  Seasonal  distribution  of  magnetite  and  ilmenite 
of  beach  sand  of  Malaga  Cove,  California;  American  Association 
of  Petroleum  Geologists  Bulletin,  v.  50,  p.  648. 

Heiskanen,  W.A.,  and  Meinesz,  F.A.,  1958,  The  earth  and  its  gravity 
field:  New  York,  McGraw-Hill,  470  p. 

Henry,  M.J.,  Berry,  R.W.,  and  Fischer,  P. J.,  1976,  Holocene  sediment 
deposits  on  the  continental  shelf,  San  Diego  County:  Geological 
Society  of  America  Abstracts  with  Programs,  v.  8,  p.  381. 

Henry,  M.J.,  1976,  The  unconsolidated  sediment  distribution  on  the 
San  Diego  County  mainland  shelf,  California;  Son  Diego  State 
University  unpublished  Master's  Thesis. 

Henyey,  T.L.,  1976,  Heat  flow  and  tectonic  patterns  on  the  southern 
California  borderland;  in  Howell,  D.G.,  editor.  Aspects  of  the 
geologic  history  of  the  Colifornia  continental  borderland;  Petro- 
leum Geologists,  Pacific  Sections,  Miscellaneous  Publication  24, 
p.  427-440. 

Henyey,  T.L.,  Teng,  T.,  and  McRaney,  J.K.,  1979,  A  sea-floor  seismic 
monitoring  network  around  on  offshore  oilfield  platform  and 
recording  of  the  August  13,  1978  Santa  Barbara  earthquake; 
Offshore  Technology  Conference,  Proceedings,  v.  4,  p.  2219- 
2223, 

Herd,  D.G.,  1978,  Intracontinentol  plate  boundary  east  of  Cope 
Mendocino,  California;  Geology,  v.  6,  no.  12,  p.  721-725. 

Herd,  D.G.,  ond  Helley,  E.J.,  1977,  Faults  with  Quaternary  displace- 
ment, northwest  San  Francisco  Boy  region,  Californio:  U.S.  Geo- 
logical Survey  Miscellaneous  Field  Studies  Mop  818,  scale 
1:125,000. 


Herron,  R.F.,  1965,  Offshore  exploration  and  developments — south- 
ern Santo  Borboro  County:  American  Associotion  of  Petroleum 
Geologists  Bulletin,  v.  49,  p.  1761. 

Hertlein,  L.G.,  1928,  Preliminary  report  on  the  poleontology  of  the 
Channel  Islands,  California;  Journol  of  Paleontology,  v.  2,  p. 
142-157. 

Hess,  G.R.,  1974,  Submorine  fanfare;  a  comporison  of  modern  and 
Miocene  deep-sea  fans;  University  of  Minnesota  unpublished 
Master's  Thesis. 

Hess,  G.R.,  and  Normark,  W.R.,  1976,  Holocene  sedimentation  his- 
tory of  the  major  fan  valleys  of  Monterey  fon:  Marine  Geology, 
V.  22,  p.  233-251. 

Hess,  G.R.,  and  Normark,  W.R.,  1980,  Quaternary  styles  of  Califor- 
nia submarine  fans;  American  Association  of  Petroleum  Geolo- 
gists Bulletin,  V.  64,  p.  443-444. 

Hess,  G.R.,  and  Normark,  W.R.,  1980,  Possible  geometries  of  sond- 
stone  bodies  as  reflected  by  geomorphic  features  on  modern 
submarine  fans:  American  Association  of  Petroleum  Geologists 
Bulletin,  V.  64,  p.  722. 

Hess,  G.R.,  Normork,  W.R.,  and  Gutmacher,  C.E.,  1979,  Sur  subma- 
rine slide,  Monterey  fan,  central  California;  Geological  Society 
of  America  Abstracts  with  Programs,  v.  11,  p.  83-84. 

Hess,  H.D.,  1979,  OCS  mining  policy  phase  II  task  force;  Progrom 
feasibility  study,  OCS  hard  minerals  leasing;  Appendix  1 1:  Pre- 
liminary resource  assessment — phosphorites  of  the  southern  Coli- 
fornia borderland;  U.S.  Geologicol  Survey  Open-File  Report  79, 
51  p. 

Hess,  H.D.,  1979,  Preliminary  resource  assessment  phosphorites  of 
the  southern  California  borderland;  U.S.  Deportment  of  Com- 
merce, National  Technical  Information  Service,  Springfield,  Vir- 
ginia, publication  number  PB  81-192635,  51  p. 

Heusser,  L.,  1978,  Pollen  in  Sonto  Borboro  basin,  California,  o  12,- 
000  year  record;  Geological  Society  of  America  Bulletin,  v.  89, 
p.  673-678. 

Higgins,  R.E.,  1973,  A  chemical  study  of  Cenozoic  volconism  in  the 
Los  Angeles  basin  and  Santa  Cruz  Island,  ond  the  Mojave  Desert: 
University  of  California,  Santo  Barbara,  unpublished  Doctoral 
Thesis. 

Hileman,  J. A.,  1979,  Seismicity  of  the  Son  Diego  region,  in  Abbott, 
P.L.,  and  Elliott,  W.J.,  editors,  Earthquokes  ond  other  perils.  Son 
Diego  region:  Son  Diego  Association  of  Geologists  Publication, 
p.  11-20. 

Hileman,  J. A.,  Allen,  C.R.,  and  Nordquist,  J.M.,  1973,  Seismicity  of 
the  southern  Californio  region  1  Januory  1932  to  31  December 
1972;  Californio  Institute  of  Technology,  Division  of  Geology  and 
Planetary  Sciences  Contribution  number  2365,  404  p. 

Hill,  D.J.,  1974,  Pre-Tertiary  rocks  observed  on  Santa  Catolino  Is- 
land, Californio;  preliminary  observations;  Geologicol  Society  of 
America  Abstracts  with  Programs,  v.  6,  p.   192. 

Hill,  D.J.,  1976,  Geology  of  the  Jurossic  basement  rocks,  Santo  Cruz 
Island,  California,  ond  correlation  with  other  Mesozoic  bosemeni 
terrains  in  California;  American  Association  of  Petroleum  Geolo- 
gists Bulletin,  V.  24,  p.  16-46. 

Hill,  G.W.,  and  Chin,  J.L.,  1982,  Mop  showing  geophysicol  trock- 
lines,  south-centrol  Monterey  Boy:  U.S.  Geological  Survey  Open- 
File  Report  82  838. 

Hill,  G.W.,  Chin,  J.L.,  and  Ho,  B.D.,  1982,  Mop  showing  surfoce  grab 
samples  and  grovity  core  locations,  south-central  Monterey  Bay, 
California  (July  19,  1981  Februory  19,  1982);  U.S.  Geological 
Survey  Open-File  Report  82-837. 

Hill,  M.L.,  1971,  Newport-lnglewood  zone  and  Mesozoic  subduction, 
Californio:  Geologicol  Society  of  America  Bulletin,  v.  82,  p. 
2957  2962. 

Holden,  Edward  S.,  1898,  A  catalogue  of  earthquokes  on  the  Pacific 
coosl;  Smithsonian  Miscellaneous  Collections  1087. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


89 


Hollister,  CD.,  Touchoke,  B.,  and  Cacchione,  D.,  1974,  Active  sedi- 
mentary processes  in  submarine  canyons:  Geological  Society  of 
America  Abstracts  with  Programs,  v.  6,  p.  799. 
Holzmon,   J.E.,    1952,   Submarine  geology  of  Cortes  and  Tanner 

banks:  Journal  of  Sedimentary  Petrology,  v.  22,  p.  97-118. 
Hopps,  T.,  and  Horon,  E.,  1984,  Subsurface  strotigrpahy:  Eel  River 
basin,  in  Hester,  R.,  and  Hallinger,  D.E.,  editors:  Selected  Papers 
of  Pacific  Section,  American  Association  of  Petroleum  Geolo- 
gists, 1983  Annual  Meeting  Sacramento,  p.  1-30  p. 
Horton,  E.E.,   1961,  Preliminary  drilling  phase  of  Mohole  Project, 
summary  of  drilling  operations:  American  Association  of  Petro- 
leum Geologists  Bulletin,  v.  45,  p.  1789-1792. 
Hoskins,  E.G.,  and  Griffiths,  J.R.,  1971,  Hydrocarbon  potential  of 
northern  and  central  California  offshore,  in  Cram,  I.H.,  editor. 
Future  petroleum  provinces  of  the  United  States — their  geology 
and  potential:  American  Association  of  Petroleum  Geologists 
Memoir  15,  p.  212-228. 
Housner,  G.W.,  and  Hudson,  D.E.,  1958,  The  Port  Hueneme  earth- 
quake of  March   18,   1957:  Seismological  Society  of  America 
Bulletin,  V.  48,  p.  163-168. 
Hov^ell,  D.G.,   1974,  Middle  Eocene  paleogeography  of  southern 
California:  University  of  California,  Santa  Barbara,  unpublished 
Doctoral  Thesis. 
Howell,  D.G.,  1975,  Eocene  paleogeography  of  southern  California 
continental    borderland:    American    Association    of    Petroleum 
Geologists,  Society  of  Economic  Paleontologists  and  Mineralo- 
gists, Annual  Meeting,  Abstracts  with  Programs,  v.  2,  p.  37-38. 
Howell,  D.G.,  1975,  The  East  Santa  Cruz  basin  fault,  southern  Cali- 
fornia continental  borderland:  Geological  Society  of  America 
Abstracts  with  Programs,  v.  7,  p.  327. 
Howell,  D.G.,  1976,  Inferred  Eocene  and  Miocene  cross  sections  of 
the  southern  California  borderland,  in  Howell,  D.G.,  editor.  As- 
pects of  the  geologic  history  of  the  California  continental  border- 
land:  American   Association   of   Petroleum   Geologists,   Pacific 
Section,  Miscellaneous  Publication  24,  p.  363-364. 
Howell,  D.G.,  1976,  Late-Miocene  counterclockwise  rotation  of  the 
south  half  of  Santa  Cruz  Island,  in  Howell,  D.G.,  editor.  Aspects 
of  the  geologic  history  of  the  California  continental  borderland: 
American  Association  of  Petroleum  Geologists,  Pacific  Section, 
Miscellaneous  Publication  24,  p.  449-454. 
Howell,  D.G.,  Crouch,  J.K.,  Greene,  H.G.,  McCulloch,  D.S.,  and 
Vedder,  J.G.,  1980,  Basin  development  along  the  late  Mesozoic- 
Cenozoic  California  margin — a  plate  tectonic  margin  of  subduc- 
tion,  oblique  subduction,  and  transform  kinematics,  in  Reading, 
H.G.,  and  Bollonce,  P.P.,  editors.  Sedimentation  along  oblique 
slip   mobile   belts:    International   Association    Sedimentologists, 
Special  Publication  no.  4,  p.  43-62. 
Howell,  D.G.,  and  Link,  M.H.,  1979,  Eocene  conglomerate  sedimen- 
tology  and  basin  analysis,  San  Diego  and  the  southern  California 
borderland:  Journal  of  Sedimentary  Petrology,  v.  49,  p.  517-539. 
Howell,  D.G.,  and  McCulloch,  D.S.,  and  Vedder,  J.G.,  1978,  Gen- 
eral geology,  petroleum  appraisal,  and  nature  of  environmental 
hazards,  eastern  Pacific  shelf,  latitude  28  degrees  to  38  degrees 
north:  U.S.  Geological  Survey  Circular  786,  29  p. 
Howell,  D.G.,  and  McLean,  H.,  1976,  Middle  Miocene  paleogeogra- 
phy, Santa  Cruz  and  Santa  Rosa  islands,  in  Howell,  D.G.,  editor, 
Aspects  of  the  geologic  history  of   the  California  continental 
borderland:  American  Association  of  Petroleum  Geologists,  Pa- 
cific Section,  Miscellaneous  Publication  24,  p.  266-293. 

Howell,  D.G.,  and  McLean,  H.,  1977,  Basin  analysis  of  provincial 
lower  and  middle  Miocene  strata,  Santa  Rosa  and  Santa  Cruz 
Islands,  California,  in  Ujiie,  H.,  and  Saito,  T.,  editors:  Proceedings 
of  the  First  International  Congress  on  Pacific  Neogene  Stratigra- 
phy, Tokyo,  Japan,  May  16-21,  1976:  Scientific  Council  of  Ja- 
pan, p.  344-345. 


Howell,  D.G.,  McLean,  H.,  and  Vedder,  J.G.,  1976,  Cenozoic  tecto- 
nism  on  Santo  Cruz  Island,  in  Howell,  D.G.,  editor.  Aspects  of  the 
geologic  history  of  the  California  continental  borderland:  Ameri- 
can Association  of  Petroleum  Geologists,  Pacific  Section,  Miscel- 
laneous Publication  24,  p.  392-416. 

Howell,  D.G.,  Stuart,  C.J.,  Piatt,  J. P.,  and  Hill,  D.J.,  1974,  Possible 
strike-slip  faulting  in  the  southern  California  borderland:  Geol- 
ogy, V.  2,  p.  93-98. 

Howell,  D.G.,  Stuart,  C.J.,  Plott,  J. P.,  and  Hill,  D.J.,  1975,  Possible 
strike-slip  faulting  in  the  southern  California  borderland.  Reply: 
Geology,  v.  3,  p.  3-4. 

Howell,  D.G.,  and  Vedder,  J.G.,  1981,  Structural  implications  of 
strotigraphic  discontinuities  across  the  southern  California  bor- 
derland, in  Ernst,  W.G.,  editor.  The  geotectonic  development  of 
California:  Prentice-Hall,  New  York,  Rubey  Colloquium,  v.  1,  p. 
535-558. 

Howell,  D.G.,  and  Vedder,  J.G.,  1984,  Ferrelo  fan,  California:  Depo- 
sitional  system  influenced  by  eustatic  sea  level  changes:  Geo- 
Marine  Letters,  v.  3,  p.  187-192. 

Howell,  D.G.,  Vedder,  J.G.,  and  McLean,  H.,  1979,  Petroleum  poten- 
tial of  a  plate  boundary:  U.S.  Geological  Survey  Professional 
Paper  1 1 50,  p.  30. 

Hoyt,  D.H.,  Geology  and  recent  sediment  distribution  from  Santa 
Barbara  to  Rincon  Point,  California:  San  Diego  State  University 
unpublished  Master's  Thesis. 

Hsu,  K.J.,  Kerry,  K.,  and  Valentine,  J.W.,  1980,  Resedimented  focies 
in  Ventura  basin,  California,  and  model  longitudinal  transport  of 
turbidity  currents:  American  Association  of  Petroleum  Geologists 
Bulletin,  v.  64,  p.  1034-1051. 

Huber,  N.K.,  1975,  Marine  terraces;  datum  planes  for  study  of 
structural  deformation:  U.S.  Geological  Survey  Earthquake  Infor- 
mation Bulletin  7:3,  p.  3-7. 

Hulsemonn,  J.,  and  Emery,  K.O.,  1961,  Stratification  in  recent  sedi- 
ments of  Santa  Barbara  basin  as  controlled  by  organisms  and 
water  character:  Journal  of  Geology,  v.  69,  p.  279-290. 

Hunter,  W.P.,  1971,  Heavy  mineral  analysis  of  selected  Monterey 
Bay  cores:  U.S.  Naval  Post  Graduate  School,  Monterey,  Califor- 
nia, unpublished  Master's  Thesis. 

Hutton,  CO.,  1959,  Mineralogy  of  beach  sands  between  Half  moon 
and  Monterey  bays,  California:  California  Division  of  Mines  and 
Geology  Special  Report  59,  32  p. 

lido,  K.,  Cos,  D.C,  and  Pararas-Coroyonnis,  G.,  1967,  Preliminary 
catalog  of  tsunamis  occurring  in  the  Pacific  Ocean:  Hawaii  Insti- 
tute of  Geophysics  Data  Report  5   (HIG  67-10). 

Inderbitzen,  A.L.,  1970,  Empirical  relationships  between  mass  physi- 
cal properties  for  recent  marine  sediments  off  southern  Califor- 
nia: Marine  Geology,  v.  9,  p.  311-329. 

Interbitzen,  A.L.,  Carsolo,  A. J.,  and  Everhort,  D.L.,  1970,  The  subma- 
rine phosphate  deposits  off  southern  California:  Offshore  Tech- 
nology Conference,  Houston,  Texas,  Paper  number  OTC  1257,  p. 
287-304. 

Ingle,  J.C,  Jr.,  1972,  Biostratigrophy  and  poleoecology  of  the  early 
Miocene  through  early  Pleistocene  benthonic  and  plonktonic 
forominifero.  Son  Joaquin  Hills,  Newport  Bay,  Orange  County, 
California,  In  Sinemeyer,  E.H.,  and  Clifford,  CC,  editors.  The 
proceedings  of  the  Pacific  Coast  Miocene  biostrotigrophic  sym- 
posium: Pacific  Section  Annual  Meeting,  Society  of  Economic 
Paleontologists  and  Mineralogists  Convention,  Bokersfield,  Cali- 
fornia, p.  255-283. 

Ingle,  J.C,  Jr.,  1974,  Oligocene  to  Holocene  plonktonic  forominifer- 
al  biofacies  and  poleoceonography  of  the  California  current 
system  at  latitude  39°  N:  Geological  Society  of  America  Ab- 
stracts with  Programs,  v.  6,  p.  195. 

Ingle,  J.C,  Jr.,  1976,  Late  Neogene  poleobathymetry  and  poleoen- 
vironments  of  the  Humboldt  basin,  northern  California,  in  Frit- 
sche,   A.E.,  Terbest,   H.,   and  Wornhardt,   W.W.,   editors.   The 


90 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


Neogene  symposium:  Society  of  Economic  Poleontologists  ond 
Mineralogists.  Pacific  Section,  Los  Angeles,  p.  53-61. 

Ingle,  J.C,  Jr.,  1977,  Cenozoic  paleoclimatic  trends,  history  of  the 
Californio  current,  and  Pacific  coast  biostrotigrophy:  Geological 
Society  of  Americo  Abstracts  with  Programs,  v.  9,  p.  1032-1033. 

Ingle,  J.C,  Jr.,  1978,  Evidence  of  latest  Miocene  refrigerotion  and 
associated  eustatic  events  in  California  and  the  North  Pacific: 
Geological  Society  of  America  Abstracts  with  Programs,  v.  10, 
p.  427. 

Ingle,  J.C,  Jr.,  1979,  Cenozoic  climatic  history  and  marine  geo- 
stratigrophy  of  the  Pacific  coast  of  North  America:  Pacific 
Sciences  Congress,  Section  Bill,  Kabarovsk  USSR,  August  1979, 
p.  63-65. 

Ingle,  J.C,  Jr.,  1979,  Correlation  of  continental-margin  and  deep- 
seo  sequences;  Neogene  examples  from  the  Pacific:  American 
Association  of  Petroleum  Geologists  Bulletin,  v.  63,  p.  473. 

Ingle,  J.C,  Jr.,  1979,  The  Humboldt  (Eel  River)  basin  of  northern 
California,  a  high  latitude  Pacific  Neogene  reference  section: 
Pacific  Science  Congress  XIV,  Section  BUI,  Kabarovsk,  USSR, 
August  1979,  p.  65-67. 

Ingle,  J.C,  Jr.,  1980,  Cenozoic  poleobathymetry  and  depositionol 
history  of  selected  sequences  within  the  southern  California  conti- 
nental borderland:  Cushmon  Foundation  Special  Publication  No. 
19,  Memorial  to  Oroville  L.  Bandy,  p.   163-195. 

Ingle,  J.C,  Jr.,  1981,  Origin  of  Neogene  diotomites  around  the 
North  Pacific  rim,  in  The  Monterey  Formation  and  related  sili- 
ceous rocks  of  California:  Society  of  Economic  Paleontologists 
and  Mineralogists,  p.  159-179. 

Ingle,  J.C,  Jr.,  ond  Keller,  G.,  1980,  Benthic  forominiferol  biofacies 
of  eastern  Pacific  margin  between  32°  South  and  32°  North: 
American  Association  of  Petroleum  Geologists  Bulletin,  v.  64,  p. 
444. 

Inmon,  D.L.,  1950,  Submarine  topography  and  sedimentation  in  the 
vicinity  of  Mugu  submarine  canyon,  California:  U.S.  Beach  Ero- 
sion Board,  Technical  Memorandum  19,  45  p. 

Inmon,  D.L.,  1954,  Beach  and  neorshore  processes  along  the  south- 
ern California  coast,  in  Johns,  R.H.,  editor.  Geology  of  southern 
California:  California  Division  of  Mines  and  Geology  Bulletin 
170,  p.  29-34. 

Inmon,  D.L.,  and  Chamberlain,  T.K.,  1960,  Littoral  sand  budget  along 
the  southern  California  coast:  Twenty-first  International  Geologi- 
cal Congress,  Copenhagen,  p.  245-246. 

Inmon,  O.L.,  and  Goldberg,  E.D.,  1963,  Petrogenesis  and  deposition- 
ol rotes  of  sediments  from  the  experimental  Mohole  drilling  off 
Lo  Jollo,  California:  American  Geophysical  Union  Transactions, 
V.  44,  p.  68. 

Isroelsky,  M.C,  1956,  Some  forominifero  from  rocks  of  Eocene  age 
on  Son  Nicolas  Island,  Ventura  County,  Colifornio:  Journal  of 
Poleontology,  v.  30,  p.  1028. 

Jochens,  R.C,  and  Griscom,  A.,  1983,  Three-dimensional  geometry 
of  the  Gordo  plate  beneath  northern  Colifornio:  Journal  of  Geo- 
physical Reseorch,  v.  88,  p.  9375-9392. 

Jackson,  P. A.,  1981,  Structural  evolution  of  the  Carpinterio  basin, 
western  Transverse  Ranges,  Colifornio:  Oregon  State  University, 
unpublished  Master's  Thesis,   107  p. 

Johns,  R.H.,  Hill,  M.L.,  LeConte,  J.,  Moore,  D.G.,  Scott,  R.F.,  Smith, 
J.L.,  ond  Smith,  S.W.,  1971,  Geologic  structure  of  the  continental 
shelf  off  Son  Onofre,  regionol  relationships  and  influence  on 
seismicity:  Unpublished  report  to  Southern  Californio  Edison 
Compony  and  Son  Diego  Gas  ond  Electric  Compony  for  consid 
erotion  in  earthquake-resistont  design  of  Units  2  ond  3  of  the  Son 
Onofre  nuclear  generating  station,  San  Clemenle,  California,  55 
P- 

Jon,  v.,  1969,  Wove  refraction  near  Son  Pedro  Bay,  California  ; 
Waterways  Harbors  Division,  Proceedings  American  Society  Civil 
Engineering,  95   (WW3),  p.  379-393. 


Jennings,  C.W.,  1959,  Geologic  mop  of  California,  Santo  Cruz 
sheet:  California  Division  of  Mines  and  Geology,  scole  1:250,- 
000. 

Jennings,  C.W.,  1959,  Geologic  mop  of  Colifornio,  Son  Luis  Obispo 
sheet:  California  Division  of  Mines  and  Geology,  scale  1:250,- 
000. 

Jennings,  C.W.,  1959,  Geologic  mop  of  California,  Santo  Maria 
sheet:  California  Division  of  Mines  and  Geology,  scole  1:250,- 
000. 

Jennings,  C.W.,  1960,  Geologic  map  of  California,  Ukioh  sheet: 
Colifornio  Division  of  Mines  and  Geology,  scale  1:250,000. 

Jennings,  C.W.,  1961,  Geologic  mop  of  California,  Son  Froncisco 
sheet:  Californio  Division  of  Mines  and  Geology,  scale  1:250,- 
000. 

Jennings,  C.W.,  1962,  Geologic  mop  of  Californio,  Long  Beoch 
sheet:  California  Division  of  Mines  ond  Geology,  scole  1:250,- 
000. 

Jennings,  C.W.,  1962,  Geologic  mop  of  Colifornio,  Redding  sheet: 
Californio  Division  of  Mines  ond  Geology,  scole  1:250,000. 

Jennings,  C.W.,  1962,  Geologic  mop  of  California,  Son  Diego  -  El 
Centro  sheet:  Colifornio  Division  of  Mines  ond  Geology,  scole 
1:250,000. 

Jennings,  C.W.,  1963,  Geologic  mop  of  Colifornio,  Santo  Roso 
sheet:  California  Division  of  Mines  and  Geology,  scale  1:230,- 
000. 

Jennings,  C.W.,  1964,  Geologic  mop  of  Californio,  Weed  sheet: 
Californio  Division  of  Mines  and  Geology,  scale  1:250,000. 

Jennings,  C.W.,  1966,  Geologic  mop  of  Californio,  Santo  Ano  sheet: 
California  Division  of  Mines  and  Geology,  scale  1:250,000. 

Jennings,  C.W.,  1975,  Preliminary  foult  ond  geologic  mop  of  south- 
ern Colifornio,  in  Crowell,  J.C,  editor.  Son  Andreas  fault  in 
southern  California:  California  Division  of  Mines  and  Geology 
Speciol  Report  118,  plate  1. 

Jennings,  C.W.,  1977,  Geologic  mop  of  Colifornio,  California  Data 
Mop  Series,  California  Division  of  Mines  ond  Geology,  scale 
1:750,000. 

Jennings,  C.W.,  and  Strand,  R.G.,  1969,  Geologic  mop  of  Colifor- 
nio, Los  Angeles  sheet:  Colifornio  Division  of  Mines  ond  Geology, 
scale  1:250,000. 

Jennings,  C.W.,  Strand,  R.G.,  Rogers,  T.H.,  Boyion,  R.T.,  Moor,  R.R., 
ond  Switzer,  R.A.,  1977,  Geologic  mop  of  California:  Colifornio 
Division  of  Mines  and  Geology,  Geologic  Data  Mop  No.  2. 

Jennings,  C.W.,  Strand,  R.G.,  Rogers,  T.H.,  Stinson,  M.C,  Burnett, 
J.L.,  Kohle,  J.E.,  ond  Streitz,  R.,  1973,  State  of  Colifornio  prelimi- 
nary foult  ond  geologic  mop,  California  Division  of  Mines  ond 
Geology. 

Jennings,  C.W.,  Strond,  R.G.,  Rogers,  T.H.,  Stinson,  M.C,  Burnett, 
J.L.,  Kohle,  J.E.,  Streitz,  R.,  Switzer,  R.A.,  ond  Moor,  R.R.,  1975, 
Foult  mop  of  Colifornio  with  locotions  of  volconoes,  thermol 
springs,  and  thermal  wells:  California  Division  of  Mines  and  Ge- 
ology, Geologic  Doto  Mop  No.  1. 

Johnson,  D.L.,  1967,  Caliche  on  the  Channel  Islands:  California  Divi- 
sion of  Mines  and  Geology,  Mineral  Information  Service,  v.  20, 
p.  151-158. 

Johnson,  D.L.,  1969,  Beochrock  (woter-toblerock)  on  Son  Miguel 
Itlond,  in  Weover,  D.W.,  editor.  Geology  of  the  northern  Chan- 
nel Islonds,  southern  Colifornio  borderland:  Americon  Associo- 
tion  of  Petroleum  Geologists,  Pacific  Sections,  p.  105-108. 

Johnson.  J  D.,  1972,  Anomalous  seismicity  on  the  continental  shelf 
of  centrol  Colifornio:  Geologicol  Society  of  Americo  Abstracts 
with  Progroms,  v.  4,  p.  554. 

Johnson.  J.W..  1974.  Bolinos  Logoon  inlet.  California:  U.S.  Army. 
Coostal  Engineering  Reseorch  Center.  Miscellaneous  Poper, 
Woshington,  DC,  No.  3-74,  46  p.,  illustrotions  (including  sketch 
mop) . 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


91 


Jones,  C.W.,  1980,  Exploring  for  oil  and  gas  on  the  continental  shelf, 
in  Yen,  T.F.,  editor.  Energy  and  resource  development  for  the 
continental  margins:  Pergamon  Press,  New  York,  p.  3-9. 

Jones,  J.H.,  1971,  General  circulation  and  water  characteristics  in 
the  southern  California  bight:  Southern  California  Water  Re- 
search Project,  SCCWRP  TRIOI. 

Jones,  D.L.,  Bloke,  M.C.,  Jr.,  and  Rangin,  C,  1976,  The  four  Jurassic 
belts  of  northern  California  and  their  significance  to  the  geology 
of  the  southern  California  borderland,  in  Howell,  D.G.,  editor. 
Aspects  of  the  geologic  history  of  the  California  continental 
borderland:  American  Association  of  Petroleum  Geologists,  Pa- 
cific Section,  Miscellaneous  Publication  24,  p.  343-362. 

Jordan,  T.H.,  Minster,  J.B.,  Christodoulidis,  D.C.,  and  Smith,  D.E., 
1985,  Constraints  on  western  U.S.  deformation  from  satellite 
loser  ranging:  Science   (in  press). 

Joy,  J.E.,  1968,  Tsunamis  and  their  occurrence  along  the  San  Diego 
County  coast:  Unpublished  report  to  the  Unified  San  Diego  Coun- 
ty Civil  Defense  and  Disaster  Organization. 

Judge,  C.W.,  1970,  Heavy  minerals  in  beach  and  stream  sediments 
OS  indicators  of  shore  processes  between  Monterey  and  Los  An- 
geles, California:  U.S.  Army  Corps  of  Engineers,  Coastal  Engi- 
neering Research  Center,  Technical  Memorandum,  33  p. 

Junger,  A.,  1974,  Source  of  the  San  Onofre  Breccia:  Geological 
Society  of  America  Abstracts  with  Programs,  v.  6,  p.  199-200. 

Junger,  A.,  1975,  Some  thoughts  on  the  structure  of  the  continental 
borderland,  southern  California:  Geological  Society  of  America 
Abstracts  with  Programs,  v.  7,  p.  331. 

Junger,  A.,  1976,  Offshore  structure  between  Santo  Cruz  and  Santa 
Rosa  Islands,  in  Howell,  D.G.,  editor.  Aspects  of  the  geologic 
history  of  the  California  continental  borderland:  American  As- 
sociation of  Petroleum  Geologists,  Pacific  Section,  Miscellaneous 
Publication  24,  p.  418-426. 

Junger,  A.,  1976,  Tectonics  of  the  southern  California  borderland,  in 
Howell,  D.G.,  editor.  Aspects  of  the  geologic  history  of  the 
California  continental  borderland:  American  Association  of  Pe- 
troleum Geologists,  Miscellaneous  Publication  24,  p.  486-498. 

Junger,  A.,  1979,  Maps  and  seismic  profiles  showing  geologic  struc- 
ture of  the  northern  Channel  Islands  platform,  California  conti- 
nental borderland:  U.S.  Geological  Survey  Miscellaneous  Field 
Studies  Mop,  MF-991,  scale  1:250,000. 

Junger,  A.,  and  Sylvester,  A.G.,  1979,  Origin  of  Emery  Seoknoll, 
southern  California  borderland:  American  Geophysical  Union 
Transactions,  v.  60,  p.  951. 

Junger,  A.,  and  Wagner,  H.C.,  1977,  Geology  of  the  Santa  Monica 
and  San  Pedro  basins,  California  continental  borderland:  U.S. 
Geological  Survey  Miscelloneous  Field  Studies  Map  MF-820, 
scale  1:250,000. 

Kalil,  F.F.,  1980,  Estimated  oil  and  gas  reserves,  southern  California 
outer  continental  shelf,  December  31,  1979:  U.S.  Geological 
Survey  Open-File  Report  80-1042,  8  p. 

Karl,  H.A.,  1975,  Bottom  and  suspended  sediments  as  indicators  of 
sedimentary  processes  operating  on  the  continental  shelf,  south- 
ern California:  Proceedings  IXth  International  Congress  of  Sedi- 
mentology,  Theme  VI,  p.  229-233. 

Karl,  H.A.,  1975,  Distribution  and  significance  of  sedimentary  struc- 
tures and  bedforms  on  the  continental  shelf,  southern  California: 
Geological  Society  of  America  Abstracts  with  Programs,  v.  7,  p. 
331-332. 

Karl,  H.A.,  1976,  Agents  of  sediment  dispersal.  Son  Pedro  continen- 
tal shelf,  southern  California:  American  Geophysical  Union 
Transactions,  v.  57,  p.  150. 

Karl,  H.A.,  1976,  Processes  influencing  transportation  and  deposi- 
tion of  sediment  on  the  continental  shelf,  southern  Californio: 
University  of  Southern  California  unpublished  Doctoral  Thesis, 
331  p. 


Karl,  H.A.,  1977,  Internal  Waves:  Implications  for  dispersal  of  sus- 
pended particulates  across  the  continental  shelf,  with  on  example 
from  southern  California:  American  Association  of  Petroleum 
Geologists,  Pacific  Section,  Miscellaneous  Publication  Annual 
Meeting,  13-16  June,  1977,  Washington,  D.C.,  Program  and 
Abstracts,  p.  63. 

Karl,  H.A.,  1977,  Origin  and  significance  of  mesoscale  current  linea- 
tions  on  the  continental  shelf,  southern  California:  Geologicol 
Society  of  America  Abstracts  with  Programs,  v.  9,  p.  443-444. 

Karl,  H.A.,  1980,  Speculations  on  processes  responsible  for  mesos- 
cale current  lineations  on  the  continental  shelf,  southern  Califor- 
nia: Marine  Geology,  v.  34,  p.  M9-M18. 

Karl,  H.A.,  1980,  Influence  of  San  Gabriel  submarine  canyon  on 
narrow-shelf  sediment  dynamics,  southern  California:  Marine  Ge- 
ology, V.  34,  p.  61-78. 

Karl,  H.A.,  Coccione,  D.A.,  and  Drake,  D.E.,  1978,  Spatial  variability 
of  the  sea-floor  and  near-bottom  water  properties  of  the  San 
Pedro  continental  shelf:  American  Geophysical  Union  Transac- 
tions, V.  59,  p.  1113-1114. 

Karl,  H.A.,  Coccione,  D.A.,  and  Drake,  D.E.,  1980,  Erosion  and 
transport  of  sediments  and  pollutants  in  the  benthic  boundary 
layer  on  the  Son  Pedro  shelf,  southern  California:  U.S.  Geologi- 
cal Survey  Open-File  Report  80-386,  54  p. 

Karl,  H.A.,  Coccione,  D.A.,  Drake,  D.E.,  and  Gorsline,  D.S.,  1980, 
Sedimentary  processes  on  the  continental  shelf  off  southern  Cali- 
fornia: American  Association  of  Petroleum  Geologists  and  Soci- 
ety of  Economic  Paleontologists  and  Mineralogists,  Abstract, 
1980  Annual  Meeting,  Denver  Colorado,  p.  74. 

Karl,  H.A.,  and  the  EEZ-SCAN,  1984,  Scientific  Team  (Cacchione, 
D.A.,  Drake,  D.E.,  Edwards,  B.D.,  Field,  M.E.,  Gardner,  J.V., 
Hampton,  M.A.,  and  McCulloch,  D.S.)  1985,  EEZ-SCAN  pro- 
gram mops  the  sea  floor:  Geotimes,  v.  30,  no.  1,  p.  13-15. 

Karl,  H.A.,  and  Plutchok,  N.B.,  1976,  Sediment  patterns  as  indicators 
of  transport  mechanics.  Son  Pedro  shelf,  California:  Geological 
Society  of  America  Abstracts  with  Programs,  v.  8,  p.  946. 

Kotz,  A.,  and  Kaplan,  I.R.,  1981,  Heavy  metals  behavior  in  coastal 
sediments  of  southern  California — A  critical  review  and  synthe- 
sis: Marine  Chemistry,  v.  10,  p.  261-299. 

Keller,  G.,  and  Ingle,  J.C,  Jr.,  1977,  Neogene  planktonic  foraminif- 
erol  biostrotigrophy  and  paleoceonography  of  the  northeastern 
Pacific:  Evidence  from  Deep  Sea  Drilling  Project  sites  173  and 
310  at  the  North  Pacific  Front:  Geological  Society  of  America 
Abstracts  with  Programs,  v.  9,  p.  1046-1047. 

Keller,  G.J.,  1957,  Distribution  of  brown  sand  off  the  coast  of  Cali- 
fornia and  Boja  California:  University  of  Southern  California 
unpublished  report  in  Marine  Geology,  19  p. 

Kelsey,  H.M.  and  Coshman,  S.M.,  1983,  Wrench  faulting  in  northern 
California  and  its  tectonic  implications:  Tectonics,  v.  2,  p.  565- 
576. 

Kemnitzer,  L.E.,  1933,  Geology  of  Son  Nicolas  and  Santo  Barbara 
Islands,  southern  California:  California  Institute  of  Technology 
unpublished  Master's  Thesis. 

Kemnitzer,  L.E.,  1936,  The  geology  of  San  Nicolas  Island,  California: 
American  Association  of  Petroleum  Geologists  Bulletin,  v.  20,  p. 
1519. 

Kennedy,  G.L.,  Lojoie,  K.R.,  and  Wchmiller,  J.F.,  1982,  Amino  stra- 
tigraphy and  founol  correlations  of  late  Quaternary  marine  ter- 
races Pacific  Coast,  USA:  Nature,  v.  299,  p.  545-547. 

Kennedy,  M.P.,  1973,  Bedrock  lithologies,  Son  Diego  coastal  area, 
California,  in  Studies  on  the  geology  and  geologic  hazards  of  the 
greater  Son  Diego  area,  California:  Son  Diego  Association  of 
Geologists,  Son  Diego,  California,  p.  9-15. 

Kennedy,  M.P.,  1973,  Stratigraphy  of  the  Son  Diego  emboyment, 
California:  University  of  California,  Riverside,  unpublished  Doc- 
toral Thesis. 


92 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


Kennedy,  M.P.,  1975,  Geolog/  of  the  San  Diego  metropolitan  area, 
California  Division  of  Mines  and  Geolog/  Bulletin  200,  p.  1-39. 

Kennedy,  MP.,  Clorke,  S.H.,  Greene,  H.G.,  and  Legg,  M.R.,  1980, 
Recency  and  character  of  faulting  offshore  metropoliton  San 
Diego,  California  (area  3  of  3,  Point  Lo  Jollo  to  Mexico) :  Califor- 
nia Division  of  Mines  and  Geology  Mop  Sheet  42. 

Kennedy,  M.P.,  Clarke,  S.H,,  Greene,  H.G.,  and  Lonsdale,  P.F., 
1985,  Observations  from  DSRV  ALVIN  of  Quaternary  foulting  on 
the  southern  California  continental  margin:  U.S.  Geological  Sur- 
vey Open-File  Report  85-39,  26  p. 

Kennedy,  M.P.,  Greene,  H.G.,  Clarke,  S.H.,  and  Bailey,  K.A.,  1980, 
Recency  and  chorocter  of  faulting  offshore  metropolitan  San 
Diego,  California  (area  2  of  3,  Point  La  Jolla  to  Cordiff-by-the- 
Seo):  California  Division  of  Mines  and  Geology  Map  Sheet  41. 

Kennedy,  M.P.,  Tan,  S.S.,  Chapman,  R.H.,  and  Chase,  T.W.,  1975, 
Character  and  recency  of  faulting.  Son  Diego  metropolitan  area, 
California:  California  Division  of  Mines  and  Geology  Special 
Report  123. 

Kennedy,  M.P.,  Welday,  E.E.,  Borchardf,  G.,  Chase,  T.W.,  and 
Chapman,  R.H.,  1977,  Studies  on  surface  faulting  and  liquefac- 
tion OS  potential  eorthquoke  hozords  in  urban  Son  Diego,  Cali- 
fornia: California  Division  of  Mines  and  Geology  final  technicol 
report  submitted  to  U.S.  Geological  Survey  contract  number 
14-08-0001-15858,  52  p. 

Kennedy,  M.P.,  and  Welday,  E.E.,  1980,  Recency  and  character  of 
faulting  offshore  metropolitan  Son  Diego,  California  [area  1  of 
3,  Son  Diego  Boy  and  immediate  offshore  shelf):  California 
Division  of  Mines  and  Geology  Map  Sheet  40. 

Kennett,  W.E.,  1944,  Geologic  mop  of  Santo  Cruz  Island:  Unpub- 
lished Superior  Oil  Company  Mop,  scale  1:46,CXX). 

Kennett,  W.E.,  1952,  Channel  Island  columnar  sections,  in  Redwine, 
L.E.,  and  others,  editors,  Cenozoic  correlation  section,  western 
Ventura  basin  from  Point  Conception  to  Ventura  and  Channel 
Islands,  California:  American  Association  of  Petroleum  Geolo- 
gists, Pacific  Section,  Geologicol  Names  and  Correlations  Com- 
mittee, Subcommittee  on  Cenozoic,  1  sheet. 

Kennett,  W.E.,  1952,  Cenozoic  correlation  section,  western  Ventura 
bosin  from  Point  Conception  to  Ventura  and  Channel  Islands, 
California:  American  Association  of  Petroleum  Geologists,  Pa- 
cific Section,  2  sheets. 

Kern,  J. P.,  1977,  Origin  and  history  of  upper  Pleistocene  morine 
terraces,  San  Diego,  California:  Geological  Society  of  America 
Bulletin,  V.  88,  p.  1553-1566. 

Kern,  J. P.,  Stump.  T.E.,  and  Dowlen,  R.F.,  1971,  An  upper  Pleistocene 
morine  fauna  from  Mission  Boy,  San  Diego,  California:  San 
Diego  Society  of  National  History  Transactions,  v.  16,  no.  15,  p. 
329-338. 

Kew,  W.S.W.,  1927,  Geologic  sketch  of  Santo  Rosa  Island,  Santa 
Barbara  County,  California:  Geological  Society  of  America  Bulle- 
tin, V.  38,  p.  645-654. 

Kheradpir,  A.,  1968,  Foraminiferal  trends  and  poleoceonogrophy  in 
late  Pleistocene-recent  cores.  Tanner  basin,  Colifornio:  University 
of  Southern  California  unpublished  Moster's  Thesis. 

Kheradpir,  A.,  1970,  Forominiferol  trends  in  the  Quaternary  of  Ton- 
ner  basin,  California:  Micropaleontology,  v.  16,  p.  102-116. 

Kilkenny,  J.E.,  1971,  Future  petroleum  potential  of  Region  2,  Pacific 
coastal  states  and  odjocent  continental  shelf  and  slope,  in  Cram, 
I.H.,  editor.  Future  petroleum  provinces  of  the  United  States — 
their  geology  ond  potential:  American  Association  of  Petroleum 
Geologists  Memoir  15,  v.  1,  p.   170-177. 

Kling,  S.A.,  1977,  Local  and  regionol  imprints  on  radiolarian  assem- 
blages from  Colifornio  coastal  basin  sediments:  Marine  Mi- 
cropoleontology,  v.  2,  p.  207-221. 

Klise,  D.H.,  1983,  Modern  sedimentation  on  the  Colifornio  continen- 
tal margin,  adjacent  lo  the  Russion  River:  MS  Thesis,  Son  Jose 
Stote  University,   134  p. 


Knebel,  H.J.,  Conomos,  T.J.,  and  Commeou,  J. A.,  1976,  Clay-minerol 
variability  in  suspended  sediments  of  Son  Francisco  boy  system: 
American  Associolion  of  Petroleum  Geologists  Bulletin,  v.  60,  p. 
689. 

Knopf,  E.C.,  1938,  Santo  Cotalino,  minerals  and  geology:  Pocific 
Minerologist,  v.  5,  p.  3-5. 

Kolpock,  R.L.,  1972.  Bottom  currents  ond  sediment  distribution  on 
the  Hueneme  shelf,  California:  American  Geophysical  Union 
Tronsoctions,  v.  53,  p.  1028. 

Kolpock,  R.L.,  1973,  Introduction  to  Santo  Barbara  Channel  region 
revisited:  Americon  Association  of  Petroleum  Geologists,  Society 
of  Economic  Paleontologists  ond  Minerologists,  and  Society  of 
Exploration  Geophysicists.  Pacific  Sections,  Guidebook,  p.  1. 

Kolpock,  R.L.,  Mottson,  J.S.,  Mark,  H.B.,  Jr.,  and  Drake,  D.E.,  1970, 
Santo  Barbara  Channel,  Colifornio  morine  environment:  Geolog- 
icol Society  America  Abstracts  with  Progroms,  v.  2,  p.  747. 

Kolpock,  R.L.,  Mottson,  J.S.,  Mark,  H.B.,  Jr.,  ond  Yu,  T.C.,  1971, 
Hydrocarbon  content  of  Santo  Borboro  Chonnel  sediments,  in 
Kolpock,  R.L.,  editor.  Biological  and  oceonogrophicol  survey  of 
the  Santo  Barbara  Channel  oil  spill  1969-1970 — Physical,  chemi- 
col,  ond  geologicol  studies:  University  of  Southern  California, 
Allan  Hancock  Foundotion,  v.  2,  p.  276-295. 

Komor,  P.D.,  1969,  The  channelized  flow  of  turbidity  currents  with 
application  to  Monterey  deep-sea  fon  channel:  Journal  of  Geo- 
physical Reseorch,  v.  74,  p.  4544-4558. 

Kososki,  B.A.,  Cavit,  CD.,  ond  McHendrie,  A.G.,  1981,  Free-air 
gravity  map  of  the  Colifornio  outer  continentol  shelf:  U.S.  Geo- 
logicol Survey  Miscelloneous  Field  Studies  Mop,  no.  MF-0854. 

Krouse,  DC,  1961,  Geology  of  the  southern  continentol  borderland 
west  of  Bojo  Colifornio,  Mexico:  University  of  Colifornio,  Son 
Diego,  Scripps  Institution  of  Oceanography  unpublished  Doc- 
torol  Thesis. 

Krouse,  D.C.,  1962,  Faulting  in  the  continental  borderland  relative 
to  the  Aguo  Blonca  fault:  Geological  Society  of  America  Speciol 
Paper  68,  p.  35. 

Krouse,  DC,  1964,  Lithology  ond  sedimentotion  in  the  southern 
continental  borderland,  in  Miller,  R.L.,  editor.  Papers  in  marine 
geology,  Shepord  Commorotive  Volume:  New  York,  MocMillon, 
p.  274-318. 

Krouse,  D.C.,  1965,  Tectonics,  bathymetry,  and  geomognetism  of 
the  southern  continentol  borderland  west  of  Bajo  Colifornio, 
Mexico:  Geological  Society  of  America  Bulletin,  v.  76,  p.  617- 
650. 

Kvenvolden,  K.A.,  1962,  Normal  paraffin  hydrocarbons  in  sediments 
from  Son  Froncisco  Boy,  California:  Americon  Associotion  of 
Petroleum  Geologists  Bulletin,  v.  46,  p.   1643. 

Kvenvolden,  K.A.,  ond  Field,  M.E.,  1981,  Thermogenic  hydrocorbons 
in  unconsolidoted  sediment  of  the  Eel  River  basin,  offshore  north- 
ern California:  American  Association  of  Petroleum  Geologists 
Bulletin,  V.  65,  p.  1642-1646. 

Kvenvolden,  K.A.,  Field,  M.E.,  and  Clorke,  S.H.,  Jr.,  1980,  Thermo- 
genic hydrocarbon  gases  in  unconsolidated  seofloor  deposits, 
northern  Colifornio  continental  margin:  Americon  Associotion  of 
Petroleum  Geologists  Bulletin,  v.  64,  p.  736. 

Kvenvolden,  K.A.,  Ropp,  J.B.,  and  Redden,  G.O.,  1979,  Hydrocar- 
bons in  sediments  on  the  flonks  of  the  Tonner  and  Cortez  bonks 
— a  preliminory  report:  Proceedings,  workshop  on  stondord  ref- 
erence materials  for  offshore  drilling — petroleum:  Notional  Bu- 
reou  of  Stondords  Speciol  Publicotion,  U.S.  Department  of 
Commerce,  Washington,  D.C. 

Lojoie,  K.R.,  Kern,  J. P.,  Wehmiller,  J  F..  Kennedy,  G.L.,  Methieson, 
S.A.,  Sorno-Wojcicki,  A.M.,  Yerkes,  R.F.,  and  McCrory,  P.F., 
1979,  Quoternory  marine  shorelines  ond  crustol  deformation  Son 
Diego  to  Sonto  Borboro,  California,  in  Abbot,  PL.,  editor.  Geo- 
logical  excursions   in   the   southern   California   oreO:    Field   Trip 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


93 


Guidebook,  no.  1,  Geological  Society  of  America    92nd  Annual 
Meeting,  p.  1-16. 

Lojoie,  K.R.,  Wehmiller,  J.,  Kvenvolden,  K.A.,  Peterson,  E.,  and 
Wright,  R.H.,  1975,  Correlation  of  California  marine  terraces  by 
amino  acid  stereochemistry:  Geological  Society  of  America  Ab- 
stracts with  Programs,  v.  7,  p.  333-334. 

Lamar,  D.L.,  Merifield,  P.M.,  and  Stout,  M.L.,  1968,  Engineering 
geology  of  rock  in  core  hole.  Eel  Point,  San  Clemente  Island, 
California:  Naval  Weapons  Center  Technical  Publication  4487, 
18  p. 

Lamb,  T.N.,  1978,  Geology,  in  Kuper,  H.T.,  and  Hart,  M.W.,  editors, 
Natural  history  of  the  Coronodo  Islands,  Boja  California,  Mexico: 
Son  Diego  Association  of  Geologists  Publication,  p.  12-44. 

Lowson,  A.C.,  1897,  The  post-Pliocene  diastrophism  of  the  coast  of 
southern  California:  University  of  California  Bulletin,  Department 
of  Geology,  v.  1,  p.  116-157. 

Lawson,  A.C.,  1924,  The  continental  shelf  off  the  coast  of  California: 
National  Research  Council  Bulletin,  v.  8,  23  p. 

Lawson,  A.C.,  1950,  Sea  bottom  off  the  coast  of  California — a 
review  of  Special  Paper  31,  Geological  Society  of  America,  by 
Shepord  and  Emery,  1941:  Geological  Society  of  America  Bulle- 
tin, v.  61,  p.  1225-1242. 

LeConte,  Joseph,  1887,  The  flora  of  the  coast  islands  of  California 
in  relation  to  recent  changes  of  physical  geography:  American 
Journal  of  Science,  v.  34,  p.  457-460. 

Lee,  H.J.,  and  Edwards,  B.D.,  1984  (in  review).  Surface  coring  to 
assess  offshore  slope  stability:  submitted  to  Journal  Geotechnical 
Engineering,  American  Society  of  Civil  Engineers,  10  figures,  1 
table,  26  p. 

Lee,  H.J.,  Edwards,  B.D.,  and  Field,  M.E.,  1981,  Geotechnical  analy- 
sis of  a  submarine  slump.  Eureka,  California:  Proceedings  Volume 
of  the  13th  Annual  Offshore  Technology  Conference,  Paper  No. 
4121,  p.  53-59,  9  figures. 

Lee,  T.C.,  1974,  Heat  flow  and  other  geophysical  studies  in  the 
southern  California  borderland:  Dissertation  Abstracts,  v.  35,  p. 
899B. 

Lee,  T.C.,  and  Henyey,  T.L.,  1975,  Heat  flow  through  the  southern 
California  borderland:  Journal  of  Geophysical  Research,  v.  80, 
p.  3733-3743. 

Lee,  W.H.K.,  Johnson,  C.E.,  Henyey,  T.L,  and  Yerkes,  R.L.,  1978,  A 
preliminory  study  of  the  Santo  Barbara,  California  earthquake  of 
August  13,  1978,  and  its  major  aftershocks:  U.S.  Geological 
Survey  Circular  797,  1  p. 

Lee,  W.H.K.,  Roller,  J.C,  Bauer,  P.G.,  and  Johnson,  J.D.,  1972a, 
Catalog  of  earthquakes  along  the  San  Andreas  fault  system  in 
central  California  for  the  year  1969;  U.S.  Geological  Survey 
Open-File  Report,  49  p. 

Lee,  W.H.K.,  Roller,  J.C,  Meagher,  K.L,  and  Bennett,  R.E.,  1972b, 
Catalog  of  earthquakes  along  the  San  Andreas  fault  system  in 
centrol  California  for  the  yeor  1970:  U.S.  Geological  Survey 
Open-File  Report,  73  p. 

Lee,  W.H.K.,  Meagher,  K.L.,  Bennett,  R.E.,  and  Motamoros,  E.E., 
1972c,  Catalog  of  earthquakes  along  the  Son  Andreas  fault 
system  in  central  California  for  the  year  1971:  U.S.  Geological 
Survey  Open-File  Report,  62  p. 

Lee,  W.H.K.,  Yerkes,  R.F.,  ond  Simirenko,  M.,  1979,  Recent  earth- 
quake activity  ond  focal  mechanisms  in  the  western  Transverse 
Ranges,  California:  U.S.  Geological  Survey  Circular  799-A,  p. 
1-26. 
Lee,  W.H.K.,  and  Vedder,  J.G.,  1973,  Recent  earthquake  activity  in 
the  Santa  Barbara  Chonnel  region:  Seismological  Society  of 
America  Bulletin,  v.  63,  p.  1757-1773. 
LeFever,  R.D.,  Anderhalt,  R.,  and  Reed,  W.E.,  1977,  Trend-surface 
analysis  of  texturol  data  from  the  southern  California  borderland: 
Geological  Society  of  America  Abstracts  with  Programs,  v.  9,  p. 
451. 


Legg,  M.R.,  1980,  Selsmicity  and  tectonics  of  the  inner  continental 
borderland  of  southern  California  and  northern  Boja  California, 
Mexico:  University  of  California,  San  Diego,  unpublished  Mas- 
ter's Thesis. 

Legg,  M.R.,  1980,  Present-day  micro-plate  tectonics  in  the  southern 
California  continental  borderland:  American  Geophysical  Union 
Abstract,  v.  61,  p.  1124. 

Legg,  M.R.,  1985,  Structure  and  tectonics  of  the  inner  continental 
borderlond  offshore  northern  Boja  Californio  Mexico:  University 
of  California,  Santo  Barbara,  unpublished  Doctoral  Dissertation. 

Legg,  M.R.,  and  Agnew,  D.C.,  1979,  The  1862  earthquake  in  San 
Diego,  in  Abbott,  P.L.,  and  Elliott,  W.J.,  editors.  Earthquakes  and 
other  perils.  Son  Diego  region:  San  Diego  Association  of  Geolo- 
gist Publication,  p.  139-142. 

Legg,  M.R.,  Agnew,  D.C.,  and  Simons,  R.S.,  1977,  Earthquake  his- 
tory and  recent  seismicity  of  coastal  Son  Diego  County,  Califor- 
nia, 1800-1976,  in  Kuhn,  G.,  editor.  Coastal  zone  geology  and 
related  sea  cliff  erosion:  San  Dieguito  River  to  San  Elijo  Lagoon, 
San  Diego  County,  California:  San  Diego  County  Board  of 
Supervisors  Project  Study  1 1596-0800E-KUHN. 

Legg,  M.R.,  and  Kennedy,  M.P.,  1979,  Faulting  offshore  San  Diego 
and  northern  Boja  California,  in  Abbott,  P.L.  and  Elliott,  W.J., 
editors.  Earthquakes  and  other  perils,  San  Diego  region:  San 
Diego  Association  of  Geologist  Publicotion,  p.  29-46. 

Legg,  M.R.,  and  Luyendyk,  B.P.,  1982,  Seabeam  survey  of  an  active 
strike-slip  fault  in  the  southern  California  continental  borderland: 
American  geophysical  Union  Transactions,  v.  63,  p.  1107. 

Legg,  M.R.,  and  Ortega,  V.W.,  1978,  New  evidence  for  major  fault- 
ing in  the  inner  borderland  off  northern  Baja  California,  Mexico: 
American  Geophysical  Union  Transactions,  v.  59,  p.  1134. 

Legg,  M.R.,  and  Wong,  V.,  1979,  Faulting  and  earthquake  risk 
offshore  southern  California  (USA)  and  nothern  Boja  California 
(Mexico),  in  Proceedings  at  the  Symposium  on  Human  Settle- 
ments of  the  San  Andreas  Fault  System:  California  Seismic 
Safety  Commission  Publication,  p.  136-151. 

Legg,  M.R.,  and  Wong,  V.,  1979,  Faulting  in  the  inner  continental 
borderland  offshore  northern  Baja  California,  Mexico:  Geologi- 
cal Society  of  America  Abstracts  with  Programs,  v.  11,  p.  464. 

Leslie,  R.B.,  1981,  Continuity  and  tectonic  implications  of  the  Sime- 
on-Hosgri  fault  zone,  central  California:  U.S.  Geological  Survey 
Open-File  Report  81-430,  64  p. 

Lester,  F.W.,  Kirkmon,  S.L.,  and  Meagher,  K.L.,  1976,  Catalog  of 
earthquakes  along  the  Son  Andreos  foult  system  in  central  Cali- 
fornia, October  -  December  1973:  U.S.  Geological  Survey  Open- 
File  Report  76-732,  37  p. 

Lester,  F.W.,  and  Meagher,  K.L.,  1978,  Catalog  of  earthquakes 
along  the  San  Andreas  fault  system  in  central  California  for  the 
year  1974;  U.S.  Geological  Survey  Open-File  Report  78-1010, 
89  p. 

Lester,  F.W.,  Meagher,  K.L.,  and  Wesson,  R.L.,  1976,  Catalog  of 
eorthquokes  along  the  San  Andreas  fault  system  in  central  Cali- 
fornia, July  -  September  1973:  U.S.  Geological  Survey  Open-File 
Report  76-169,  38  p. 

Lewis,  K.B.,  1971,  Slumping  on  a  continental  slope  inclined  at  1°  - 
4°:  Sedimentology,  v.  16,  p.  97-110. 

Limerick,  S.H.,  1978,  Animal-sediment  relotionships  of  Tanner  and 
Cortes  banks,  California  continental  borderland;  Geological  So- 
ciety of  America  Abstracts  with  Programs,  v.  10,  p.  444-445. 

Lipman,  P.W.,  Prostko,  H.J.,  and  Christiansen,  R.L.,  1971,  Evolving 
subduction  zones  in  the  western  United  States,  as  interpreted 
from  igneous  rocks;  Science,  v.  174,  p.  821-825. 

Lipps,  J.H.,  1964,  Late  Pleistocene  history  of  west  Anocopo  Island, 
California:  Geological  Society  of  America  Bulletin,  v.  75,  p. 
1169-1176. 

Lipps,  J.H.,  1964,  Miocene  plonktonic  forominifero  from  Newport 
Bay,  California:  Tulane  Studies  in  Geology,  v.  2,  p.  109-133. 


94 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


lipps,  J.H.,  1967,  Age  and  environment  of  marine  terrace  fauna,  Son 
Clemente  liland,  California:  The  Veliger,  v.  9,  p.  388-398. 

Lipps,  J.H.,  Valentine,  J.W.,  and  Mitchell,  E.,  1968,  Pleistocene 
poleoecology  and  bioslrctigraphy,  Santo  Barbara  Island,  Cali- 
fornia: Journal  of  Paleontology,  v.  42,  p.  291-307. 

Lohmor,  J.M.,  and  Worme,  J.E.,  1978,  Anotomy  of  on  Eocene  sub- 
morine  canyon-fan  system,  southern  California  borderland:  Off- 
shore Technology  Conference,  v.  1,  p.  571-580. 

Lonsdale,  P.,  1979,  A  deep-sea  hydrothermol  site  on  a  strike-slip 
fault   (Son  Clemente  Foult):  Noture,  v.  281,  p.  531-534. 

Loughridge,  M.S.,  1968,  Fine-scale  topography  and  magnetic  ono- 
molies  of  the  deep  sea  floor  off  southern  California:  Scripps 
Institution  of  Oceanography,  SIO  Reference  78-2,  67  p. 

Ludwick,  J.C,  Jr.,  1950,  Deep-water  sand  layers  off  San  Diego, 
California:  University  of  California,  Los  Angeles,  unpublished 
Doctoral  Thesis. 

Luyendyk,  B.P.,  Hajic,  E.J.,  end  Simonett,  D.A.,  1983,  Side-SCAN 
sonar  mapping  and  computer-aided  interpretation  in  the  Sonto 
Barbara  Channel,  California:  University  of  California  Santa  Bar- 
bora  Report  No.  T-CSGCP-006  (California  Sea  Grant  Program) . 

Luyendyk,  B.P.,  Komerling,  M.J.,  and  Terres,  R.R.,  1980,  Geometric 
model  for  Neogene  crustol  rotations  in  southern  Coiifornia:  Geo- 
logical Society  of  America  Bulletin,  v.  91,  p.  211-217. 

Luyendyk,  B.P.,  Komerling,  M.J.,  Terres,  R.R.,  and  Hornofius,  J.S., 
1985,  Simple  sheor  of  southern  California  during  Neogene  time 
suggested  by  poleomognetic  declinations:  Journal  of  Geophysi- 
cal Research,    (in  press). 

Luken,  MD.  and  Hess,  H.D.,  1979,  Sand,  gravel,  and  shell  deposits 
of  the  southern  California  borderland:  U.S.  Geological  Survey, 
Appendix  10,  OCS  Mining  Policy  Phase  II,  task  force  program 
feasibility  document,  69  p. 

MacDonold,  K.B.,  Hones,  S.D.,  Howder,  W.J.,  and  Jordon,  P.C, 
1976,  Shell  assemblages  and  biogenic  sedimentary  structures 
from  the  Sonto  Barbara  basin,  California  borderland:  Geological 
Society  of  America  Abstrocts  with  Programs,  v.  8,  p.  990-991. 

Mohmood,  A.,  and  Reifel,  M.D.,  1978,  Foundation  conditions  in 
outer  banks  area  offshore  southern  California:  Offshore  Technol- 
ogy Conference,  Proceedings,  v.  2,  p.   1401-1408. 

Moloney,  N.J.,  and  Alba,  C.A.,  1978,  Oriented  coastal  erosion  pat- 
terns and  pocket  beach  formolion.  Corona  Del  Mar,  California: 
American  Geophysical  Union  Transactions,  v.  59,  p.  1114. 

Moloney,  N.J.,  and  McGlothlin,  J.S.,  1979,  Neorshore  sedimenta- 
tion on  a  pocket  beach.  Crescent  Beach,  California:  Geological 
Society  of  Americo  Abstracts  with  Programs,  v.   11,  p.  89-90. 

Moloulo,  D.N.,  1978,  Holocene  sedimentation  in  Sonto  Monica  bo- 
sin,  Coiifornia:  University  of  Southern  California  unpublished 
Master's  Thesis. 

Molouta,  D.N.,  Gorsline,  D.S.,  and  Friedman,  G.M.,  1978,  Sedimen- 
tary processes  and  rotes  in  margin  basins,  California  continental 
borderland:  Tenth  Inlernotionol  Congress  on  Sedimentology,  Je- 
rusalem, Isroel,  July  9-14,   1978,  p.  405-410. 

Molouta,  D.N.,  Gorsline,  D.S.,  and  Thornton,  S.E.,  1981,  Processes 
and  rotes  of  recent  (Holocene)  basin  filling  in  on  active  trans- 
form margin:  Sonto  Monica  bosin,  California  continental  border 
land:  Journal  of  Sedimentary  Petrology,  v.  51,  p.   1077-1095. 

Marks,  S.M.,  and  Fluty,  L.,  1981,  Cotolog  of  eorthquokes  along  the 
Son  Andreas  fault  system  in  central  California,  July  -  September 
1977:  US    Geological  Survey  Open. File  Report  81  462,  43  p. 

Marks,  S  M  ,  and  Lester,  F  W.,  1980o,  Catalog  of  eorthquokes  along 
the  Son  Andreas  foult  system  in  centrol  Colifornio,  January 
March  1977:  U.S.  Geological  Survey  Open  File  Report  80  1233, 
47  p. 

Marks,  S.M.,  and  Letter,  F.W.,  1980b,  Catalog  of  earthquakes  along 
the  Son  Andreas  fault  system  in  central  California,  April  -  June 
1977:  U.S.  Geological  Survey  Open  File  Report  80  1264,  47  p. 


Morlette,  J.W.,  1954,  The  breakwater  at  Redondo  Beoch,  California, 
ond  its  effects  on  erosion  and  sedimentation:  University  of  South- 
ern California  unpublished  Master's  Thesis. 

Marshall,  N.F.,  1976,  Large  sediment  slump  reopens  unknown 
Scripps  submarine  canyon  tributary:  Americon  Association  of 
Petroleum  Geologists  Bulletin,  v.  60,  p.  695. 

Martin,  B.D.,  1964,  Monterey  submarine  canyon,  Coiifornia:  Genesis 
and  relationship  to  continental  geology:  University  of  Southern 
California  unpublished  Doctoral  Thesis. 

Martin,  B.D.,  and  Emery,  K.O.,  1967,  Geology  of  Monterey  Conyon, 
California:  American  Association  of  Petroleum  Geologists  Bulle- 
tin, V.  51,  p.  2281-2304. 

Martindole,  S.G.,  and  Hess,  H.D.,  1979,  Resource  assessment  of 
sand,  grovel,  and  shell  deposits  on  the  continental  shelf  of  north- 
ern and  central  Coiifornia:  U.S.  Department  of  Commerce, 
Springfield,  Virginia,  U.S.  Department  of  Commerce,  Notional 
Technical  Information  Service  Publication  Number  PB  81- 
192601,  39  p. 

Mason,  R.G.,  and  Raff,  A.D.,  1961,  A  magnetic  survey  off  the  west 
coast  of  North  America,  32  degrees  N  to  42  degrees  N:  Geologi- 
cal Society  of  Americo  Bulletin,  v.  72,  p.   1259-1265. 

Mattel,  A.D.,  1917,  Two  Santo  Barbara  Channel  earthquakes:  Seis- 
mological  Society  of  America  Bulletin,  v.  7,  p.  61-66. 

Mottinson,  J.M.  and  Hill,  D.J.,  1976,  Age  of  plutonic  basement 
rocks,  Santo  Cruz  Island,  California,  in  Howell,  D.G.,  editor. 
Aspects  of  the  geologic  history  of  the  California  continental 
borderland:  American  Association  of  Petroleum  Geologists,  Pa- 
cific Section,  Miscellaneous  Publication  24,  p.  53-59. 

Moytum,  J.R.,  and  Elliott,  W.J.,  1970,  Upper  Cretaceous  stroto  of 
the  Lo  Jollo-Point  Lomo  area,  San  Diego — Correlation  and  physi- 
cal stratigraphy,  in  Pacific  slope  geology  of  northern  Bojo  Coii- 
fornia and  adjacent  Alto  California:  American  Association  of 
Petroleum  Geologists,  Society  of  Economic  Paleontologists  ond 
Mineralogists,  ond  Society  of  Explorofion  Geophysicists,  Pacific 
Sections,  Guidebook,  p.  38-52. 

Moyugo,  M.N.,  1970,  Geology  and  development  of  California's 
giant — Wilmington  Field,  in  Geology  of  Giant  Petroleum  Fields: 
American  Association  of  Petroleum  Geologists  Memoir  14,  p. 
158  184. 

Moyugo,  M.N.,  and  Allen,  D.R.,  1966,  Long  Beoch  subsidence,  in 
Engineering  geology  in  southern  California:  Association  of  Engi- 
neering Geologists,  Los  Angeles  Section,  Special  Publicotion,  p. 
281-285. 

McCulloch,  D.S.,  1976,  Acoustic  reflection  profiles,  R  V  KELEZ,  April 
1973,  Leg  1,  Gulf  of  Forollones,  centrol  California  offshore:  U.S. 
Geologicol  Survey  Open-File  Report  76-736,  50  p. 

McCulloch,  D.S.,  1976,  Acoustic  reflection  profiles,  R  V  LEE,  Novem- 
ber, 1975,  Leg  1,  Cormel  Boy  to  Son  Luis  Boy,  central  California 
offshore:  U.S.  Geologicol  Survey  Open  File  Report  76-180,  50  p. 

McCulloch,  D.S.,  1979.  Report  of  dive  number  947  of  submersible 
ALVIN  in  the  Sonto  Barbara  Chonnel,  Colifornio,  2  August,  1979: 
Unpublished  report  to  the  Colifornio  Division  of  Mines  ond  Geol- 
ogy. 

McCulloch,  D.S.,  editor,  1980,  A  summary  report  of  the  regional 
geology,  environmental  geology,  OCS  resource  opproisol,  petro- 
leum potential,  ond  operational  considerations  in  the  area  of 
proposed  Lease  Sole  73,  offshore  Colifornio:  US  Geological 
Survey  Open-File  Report  80-2007,   142  p. 

McCulloch,  D  S.,  1980,  Faults  and  late  Miocene  folds  in  the  offshore 
Sonto  Mario  Basin  Point  Arguello  oreo,  Colifornio,  for  U.S.  Bu- 
reau of  lond  Management  report,   1  mop,  scole  1:250,000. 

McCulloch,  D.S.,  1980,  Mop  of  surface  and  neor-surfoce  geologic 
features  in  offshore  Sonto  Mario  basin,  California  for  U.S.  Bu- 
reau of  lond  Monogemenl  report.   1   mop,  scole  1  250,000. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


95 


McCulloch,  D.S.,  1982,  Geohazards  in  OCS  Lease  Sale  73,  central 
California:  U.S.  Geological  Survey  Administrative  Report,  25  p. 
13  maps,  scale  1:250,000. 

McCulloch,  D.S.,  1984,  The  geology  beneath  Drakes  Boy,  in  Murphy, 
L.,  editor.  Submerged  cultural  resources  survey  portions  of  Point 
Reyes  Notional  Seashore  and  Point  Reyes  National  Seashore 
and  Point  Reyes-Forollon  Islands  National  Marine  Sanctuary: 
Southwest  Cultural  Resources  Center  Professional  Paper  No.  1, 
National  Pork  Service,  U.S.  Department  of  Interior,  Santa  Fe, 
Uew  Mexico,  p.  123-139. 

McCulloch,  D.S.,  1985,  Evoluating  tsunami  hazard,  in  Ziony,  J. I., 
editor.  Evaluating  earthquake  hazards  in  the  Los  Angeles  region 
— an  earth-science  perspective:  U.S.  Geological  Survey  Profes- 
sional Paper  1360. 

McCulloch,  D.  S.,  1987,  Regional  geology  and  hydrocarbon  poten- 
tial of  offshore  central  California,  in  Scholl,  D.  W.,  Grantz,  A., 
and  Vedder,  J.  G.,  editors.  Geology  and  resource  potential  of  the 
continental  margin  of  v/estern  North  America  and  adjacent 
ocean  basins — Beaufort  Sea  to  Bajo  California:  Circum  Pacific 
Council  for  Energy  and  Mineral  Resource,  Earth  Science  Series 
(in  press) . 

McCulloch,  D.S.,  and  Chapman,  R.H.,  1977,  Residual  magnetic  in- 
tensity maps  along  the  California  coast  from  37  degrees  30 
minutes  latitude  to  34  degrees  30  minutes  latitude:  U.S.  Geologi- 
cal Survey  Open-File  Report  77-79,  14  aeromagnetic  maps,  1:- 
125,000. 

McCulloch,  D.S.,  Clarke,  S.H.,  Dolton,  G.L.,  Field,  M.E.,  Scott,  E.W., 
and  Utter,  P. A.,  1982,  Geology  environmental  hazards,  and  pe- 
troleum resources  for  1982  OCS  Lease  Sale  73:  U.S.  Geological 
Survey  Open-File  Report  82-1000. 

McCulloch,  D.S.,  Clarke,  S.H.,  Jr.,  Field,  M.E.,  Scott,  E.W.,  and  Utter, 
P.M.,  1977,  A  summary  report  of  the  regional  geology,  petroleum 
potential,  and  environmental  geology  of  the  southern  proposed 
Lease  Sale  53,  northern  California  outer  continental  shelf:  U.S. 
Geological  Survey  Open-File  Report  77-593,  59  p. 

McCulloch,  D.S.,  Clarke,  S.H.,  Field,  M.E.,  and  Utter,  P.A.,  1980, 
Regional  geology,  petroleum  potential,  and  environmental  geol- 
ogy in  the  northern  port  of  proposed  Lease  Sale  73,  offshore 
central  and  northern  California,  in  McCulloch,  D.S.,  editor,  U.S. 
Geological  Survey  Open-File  Report  80-2007,  Chapter  B.,  p. 
B1-B68. 

McCulloch,  D.S.,  Gardner,  J.V.,  Eittreim,  S.L.,  and  Masson,  D.G., 
1984,  GLORIA  survey  of  the  morphology  of  the  mid-Californio 
continentol  margin  out  to  200  nautical  miles:  American  Geologi- 
cal Union,  Foil  Meeting,  Son  Francisco,  EOS,  v.  65,  no.  45,  p. 
1083. 

McCulloch,  D.S.,  Greene,  H.G.,  Heston,  K.S.,  and  Rubin,  D.M., 
1980,  A  summary  report  of  the  geology  and  geologic  hazards  in 
proposed  Lease  Sale  53,  central  Californio  outer  continental 
shelf:  U.S.  Geological  Survey  Open-File  Report  80-1095,  69  p. 

McCulloch,  D.S.,  Long,  A.T.,  and  Utter,  P. A.,  1977,  Acoustic  profiles 
offshore  Humboldt  Boy,  California;  U.S.  Gological  Survey  Open- 
File  Report  77-677,  1  p. 

McCulloch,  D.S.,  Long,  A.T.,  and  Utter,  P. A.,  1977,  Faulting  in 
coastal  south-central  California:  U.S.  Geological  Survey  Profes- 
sional Paper  1100,  p.  150-151. 

McCulloch,  D.S.,  Rubin,  D.M.,  and  Clarke,  S.H.,  Jr.,  1977,  Faults 
offshore  of  Eureka,  Californio:  U.S.  Geological  Survey  Adminis- 
trative Report,  mop  scale  1:250,000. 

McCulloch,  D.S.,  Utter,  P. A.,  and  Menock,  J.,  1985,  Mops  showing 
location  of  selected  pre-Quoternory  rock  samples  from  34°  30'N 
latitude  to  42°  N  latitude,  Californio  continental  margin:  U.S. 
Geological  Survey  Miscellaneous  Field  Investigotion  Mop,  MF 
1719   (in  press). 

McCulloch,  D.S.,  Vedder,  J.G.,  Wagner,  H.C.,  and  Brune,  J.N., 
1979,  Geologic  setting,  in  Cook,  H.E.,  editor.  Geologic  studies 


of  the  Point  Conception  Deep  Stratigraphic  Test  Well  OCS-CAL 
78-164  no.  1,  outer  continental  shelf,  southern  California,  United 
States:  U.S.  Geological  Survey  Open-File  Report  79-1218,  p. 
10-25. 

McCulloh,  T.H.,  1960,  Gravity  variations  and  the  geology  of  the  Los 
Angeles  basin,  California:  U.S.  Geological  Survey  Professional 
Paper  400-B,  p.  B320-B325. 

McCulloh,  T.H.,  1969,  Geologic  characteristics  of  the  Dos  Cuodros 
offshore  oil  field,  in  Geology,  petroleum  development  and  seis- 
micity  of  the  Santo  Barbara  Channel  region,  California:  U.S. 
Geological  Survey  Professional  Paper  679-C,  p.  29-46. 

McCulloh,  T.H.,  and  Beyer,  L.A.,  1979,  Geothermal  gradients,  in 
Cook,  H.E.,  editor.  Geologic  studies  of  the  Point  Conception 
Deep  Stratigraphic  Test  Well  OCS-CAL  78-164,  no.  1,  outer 
continental  shelf,  southern  California,  United  States:  U.S.  Geo- 
logical Survey  Open-File  Report  79-1218,  p.  43-48. 

McEuen,  R.D.,  and  Pickney,  C.J.,  1972,  Seismic  risk  in  San  Diego: 
San  Diego  Society  of  Natural  History  Transactions  17,  p.  33-62. 

McEvilly,  T.V.,  1968,  Seafloor  mechanics  north  of  Cape  Mendocino, 
California:  Nature,  v.  220,  p.  901-903. 

McGlasson,  R.H.,  1957,  Foraminiferal  biofacies  around  Santo 
Catalina  Island:  University  of  Southern  California  unpublished 
Master's  Thesis. 

McHugh,  C.A.,  and  Lester,  F.W.,  1978,  Catalog  of  earthquakes 
along  the  San  Andrea  fault  system  in  central  California  for  the 
year  1976:  U.S.  Geological  Survey  Open-File  Report  78-1051, 
91  p. 

McHugh,  C.A.,  and  Lester,  F.W.,  1979,  Catalog  of  eorthquokes 
along  the  Son  Andrea  fault  system  in  central  California  for  the 
year  1975:  U.S.  Geological  Survey  Open-File  Report  79-1138, 
91  p. 

McKenzie,  D.P.,  and  Morgan,  W.J.,  1969,  Evolution  of  triple  junc- 
tions: Nations,  v.  224,  p.  125-133. 

McLaughlen,  R.J.,  Lojoie,  K.R.,  Sorg,  D.H.,  Morrison,  S.D.,  and 
Wolfe,  J.A.,  1983,  Tectonic  uplift  of  a  middle  Wisconsin  marine 
platform  near  the  Mendocino  triple  junction,  California:  Geology 
V.  11,  p.  35-39. 

McLean,  H.,  1976,  Block  fault  model  of  Santa  Cruz  Island,  in  Howell, 
D.G.,  editor.  Aspects  of  the  geologic  history  of  the  California 
continental  borderland:  American  Association  of  Petroleum 
Geologists,  Pacific  Section,  Miscellaneous  Publication  24,  p.  560- 
561. 

McLean,  H.,  Crowe,  B.M.,  and  Howell,  D.G.,  1976,  Source  of  Blanco 
Formation  volcaniclostic  rocks  and  strike-slip  faulting  on  Santo 
Cruz  Island,  in  Howell,  D.G.,  editor.  Aspects  of  the  geologic 
history  of  the  California  continental  borderland:  American  As- 
sociation of  Petroleum  Geologists  Pacific  Section,  Miscellaneous 
Publication  24,  p.  294-308. 

McLean,  H.,  and  Howell,  D.G.,  1976,  Elements  of  tectonism  deduced 
from  Miocene  strata,  northern  Channel  islands,  California,  in 
Fritsche,  A.E.,  Best,  H.T.,  and  Wornordt,  W.W.,  editors,  the  Neo- 
gene  symposium:  Pacific  Section  BSPM,  Son  Francisco,  p.  17. 

McLean,  H.,  and  Howell,  D.G.,  1984,  Miocene  Blanco  Fan,  northern 
chonnel  islonds,  California:  small  fans  reflecting  tectonism  and 
volconism:  in  Boumo,  A.H.,  editor-in-chief,  Geo-Morine  Letters, 
V.  3,  no.  2-4,  p.  161-166. 

McLean,  H.,  Howell,  D.G.,  and  Vedder,  J.G.,  1975,  Poleogeographic 
implications  of  the  Miocene-basement  unconformity,  Santo  Cruz 
Island,  California:  Geological  Society  of  Americo  Abstracts,  with 
Programs,  v.  7,  p.  346. 

McLean,  H.,  Howell,  D.G.,  and  Vedder,  J.G.,  1976,  Miocene  strata 
on  Santo  Cruz  and  Sonta  Rosa  Islands — A  reflection  of  tectonic 
events  in  the  southern  California  borderlond,  in  Howell,  D.G., 
editor.  Aspects  of  the  geologic  history  of  the  California  continen- 
tal borderlond:'  American  Association  of  Petroleum  Geologists, 
Pacific  Section,  Miscellaneous  Poblicotion  24,  p.  241-253. 


96 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


McMonus.  D.A.,  1965,  Blanco  frocfure  zone,  northeost  Pocific 
Ocean:  Morine  Geology,  v.  3,  429  p. 

McMonus,  D.A.,  1967,  Physiogrophy  of  Cobb  and  Gorda  Rises, 
northeast  Pocific  Ocean;  Geological  Society  of  Americo  Bulletin, 
V.  78,  p.  527-546. 

Menard,  H.W.,  1955,  Deformation  of  the  northeastern  Pacific  bosin 
and  the  west  coast  ol  North  America:  Geological  Society  of 
America  Bulletin,  v.  66,  p.  1149-1198. 

Menard,  H.W.,  1955,  Deep-sea  channels,  topography,  ond  sedimen- 
totion:  Americon  Association  of  Petroleum  Geologists  Bulletin  v. 
39,  p.  236-255. 

Menard,  H.W.,  1960,  Possible  pre-Pleistocene  deep-sea  fans  off 
central  California:  Geological  Society  of  America  Bulletin,  v.  71, 
p.  1271-1278. 

Menard,  H.W.,  1964,  Marine  Geology  of  the  Pacific:  New  York, 
McGrow-Hill,  271  p. 

Menard,  H.W.,  and  Dietz,  R.S.,  1952,  Mendocino  submarine  escarp- 
ment: Journal  of  Geology,  v.  60,  p.  266-278. 

Merifield,  P.M.,  and  Lomor,  D.L.,  1967,  Engineering  geology  of 
central  Son  Clemente  Island:  Naval  Weapons  Center  NWC 
TP4469,  16  p. 

Merifield,  P.M.,  Lomor,  D.L.,  and  Stout,  M.L.,  1971,  Geology  of 
central  Son  Clemente  Island,  California:  Geological  Society  of 
Americo  Bulletin,  v.  82,  p.  1989-1994. 

Mero,  J.L.,  1961,  Sea  floor  phosphorites:  California  Division  of 
Mines  and  Geology,  Mineral  Information  Service,  v.  14,  p.  1-12. 

Merschot,  W.R.,  1969,  Lower  Tertiary  poleocurrent  trends,  Santa 
Cruz  Island,  California:  American  Association  of  Petroleum 
Geologists  Bulletin  v.  53,  p.  461. 

Merselis,  W.B.,  1962,  Late  Pleistocene  shorelines  of  southern  Colifor- 
nio:  University  of  Southern  California  unpublished  Master's  The- 
sis. 

Mikoloj,  P.G.,  Schlueter,  R.S.,  and  Allen,  A. A.,  1972,  Investigation 
of  the  nature,  extent,  and  fate  of  natural  oil  seepage  off  southern 
California:  Fourth  Annual  Offshore  Technology  Conference, 
Houston,  Texas,  v.  1,  p.  365-380. 

Milow,  E.D.,  1957,  La  Jollo  ond  San  Diego  basins,  western  Son 
Diego  County,  California:  Society  of  Economic  Poleontologists 
and  Mineralogists,  Pacific  Section  Guidebook,  10  p. 

Minord,  C.R.,  Jr.,  1964,  The  erosional  ond  depositional  history  of  a 
portion  of  the  coast  of  northern  California:  University  of  Califor- 
nia, Berkeley  Hydraulic  Engineering  Laborotory  Report,  HEL  2- 
10,  63  p. 

Minord,  C.R.,  Jr.,  1971,  Quaternory  beaches  and  coosts  between  the 
Russian  River  ond  Droke's  Boy,  California:  University  of  Colifor- 
nia,  Berkeley  Hydraulic  Engineering  Laboratory  Report,  HEL  2- 
35,  206  p. 

Minch,  J. A.,  1975,  Tronspeninsulor  faulting  and  the  continentol  bor- 
derland: Geological  Society  of  America  Abstracts  with  Programs, 
V.  7,  p.  350. 

Minch,  J. A.,  Gibson,  K.N.,  ond  Peterson,  G.L.,  1976,  Closl  popula- 
tions in  Sespe  and  Powoyo  conglomerates  and  their  possible 
bearing  on  the  tectonics  of  the  southern  Colifornio  borderland, 
in  Howell,  D.G.,  editor.  Aspects  of  the  geologic  history  of  the 
California  continental  borderland:  American  Associotion  of  Pe- 
troleum Geologists,  Pocific  Section,  Miscellaneous  Publication 
24,  p.  256-265 
Minch,  J. A.,  and  James,  A.H.,  1975,  Diapiric  intrusions  and  basin 
formotion  in  the  continental  borderland,  in  Weaver,  D.W.,  Hor 
nadoy,  G.R.,  and  Tipton,  A.,  editors.  Conference  on  future  ener 
gy  horizons  of  the  Pocific  coosi,  Poleogene  symposium  and 
selected  technical  papers:  American  Association  of  Petroleum 
Geologists,  Pacific  Section,  p.  360-366. 
Minster,  J.B.,  and  Jordan,  T.H.,  1984,  Vector  constrointt  on  Ouoler 
nory  deformation  of  the  western  United  Stotes  east  and  west  ol 
the  San  Andreas  foult,  in  Crouch,  J.K.,  and  Bochmon,  SB.,  edi 


tors.  Tectonics  and  sedimentotion  along  the  Colifornio  morgin: 
Pacific  Section  SEPM,  v.  38,  p.  1-16. 

Mitchell,  ED.,  Jr.,  1963,  Contributions  from  the  Los  Angeles  Museum 
Channel  Islands  Biological  Survey  37 — Brochydont  desmostylion 
from  Miocene  of  Son  Clemente  Islond,  Colifornio:  Southern  Coli- 
fornio Acodemy  of  Sciences  Bulletin,  v.  62,  p.  192-201. 

Mitchell,  E.D.,  Jr.,  1965,  Fossil  collecting  on  Son  Clemente  Islond: 
Pacific  Discovery,  v.   18,  p.  2-8. 

Mitchell,  E.D.,  Jr.,  and  Lipps,  J.H.,  1964,  Miocene  marine  vertebrates 
from  Son  Clemente  Island,  California:  Geological  Society  of 
America  Special  Paper  76,  p.  214-215. 

Mitsushio,  H.,  Gorsline,  D.S.,  Edwards,  B.D.,  and  Yosudo,  Y.,  1978, 
Bottom  sediments  of  Son  Nicolas  basin,  California:  American 
Association  of  Petroleum  Geologists  Bulletin  v.  622,  p.  544. 

Moody,  G.B.,  1935,  The  geology  of  Santo  Rosa  Islond:  American 
Association  of  Petroleum  Geologists  Bulletin  v.  19,  p.  136. 

Moody,  J.D.,  and  Hill,  M.J.,  1956,  Wrench  fault  tectonics:  Geologi- 
cal Society  of  Americo  Bulletin,  v.  67.  p.   1207-1246. 

Moore,  D.G.,  1954,  The  marine  geology  of  Son  Pedro  Bay:  Univer- 
sity of  Southern  California,  Los  Angeles,  unpublished  Master's 
Thesis. 

Moore,  D.G.,  1954,  Submarine  geology  of  Son  Pedro  Shelf:  Journal 
of  Sedimentary  Petrology,  v.  24,  p.   162-181. 

Moore,  D.G.,  1957,  Acoustic  soundings  of  Quaternary  morine  sedi- 
ments off  Point  Lomo,  California:  U.S.  Navy  Electronics  Labora- 
tory Research  Report  815,  17  p. 

Moore,  D.G.,  1960,  Acoustic  reflection  studies  of  the  continental 
shelf  and  slope  off  southern  California:  Geologicol  Society  of 
America  Bulletin,  v.  71,  p.   1121-1136. 

Moore,  D.G.,  1961,  Submarine  slumps:  Journal  of  Sedimentory  Pe- 
trology, v.  31,  p.  343-357. 

Moore,  D.G.,  1963,  Geological  observations  from  the  bothyscoph 
Trieste  neor  the  edge  of  the  continental  shelf  off  San  Diego, 
California:  Geological  Society  of  America  Bulletin,  v.  74,  p. 
1057- 1062. 

Moore,  D.G.,  1964,  Shear  strength  and  related  properties  of  sedi- 
ments from  experimental  Mohole  (Guadalupe  site):  Journal  of 
Geophysical  Research,  v.  69.  p.  4271-4291. 

Moore,  D.G.,  1965,  Erosional  channel  wall  in  La  Jollo  sea-fan  valley 
seen  from  bothyscoph  Trieste  II:  Geologicol  Society  of  America 
Bulletin,  V.  76,  p.  385-392. 

Moore,  D.G.,  1966,  Structure,  litho-orogenic  units,  ond  postorogenic 
bosin  fill  by  reflection  profiling — California  continentol  border- 
land: U.S.  Navy  Electronics  Loborotory.  Son  Diego,  Colifornio. 
151  p. 

Moore.  D.G.,  1969,  Reflection  piafiling  studies  of  Itte  California 
continental  borderland:  Structure  ond  Quaternary  turbidite  bo- 
sins,  Geological  Society  of  America  Speciol  Paper  107.  142  p. 

Moore,  D.G.,  and  Shumwoy,  G.,  1959.  Sediment  thickness  ond 
physical  properties.  Pigeon  Point  shelf,  Colifornio:  Journal  of 
Geophysical  Research,  v.  64.  p.  367-374. 

Moore,  G.T..  1969,  Interoction  of  rivers  ond  oceans — Pleistocene 
petroleum  potential:  American  Associotion  of  Petroleum  Geolo- 
gists Bulletin  V.  53,  p.  2421-2430 

Moore,  G  W..  1970.  Seo-floor  spreading  at  the  junction  between 
Gordo  Rise  and  Mendocino  Ridge:  Geological  Society  of  Ameri- 
ca Bulletin.  V.  81,  p.  2817  2824 

Moore,  G.W..  1970.  Preliminary  appraisal  of  the  geologic  environ- 
ment offshore  from  Los  Angeles:  U.S.  Geological  Survey  Adminis- 
trative Report.  23  p. 

Moore.  G  W  .  1972,  Offshore  extension  of  the  Rose  Canyon  foult. 
Son  Diego,  Colifornio:  U.S.  Geologicol  Survey  Professionol  Po- 
per  800  C,  p    CI  13  CI  16. 

Moore,  G.W.,  1975,  Acoustic  reflection  profiles,  R  V  POLARIS,  No- 
vember-December,  1970,  offshore  soutftem  Colifornio,  Port  Hu*- 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


97 


neme  to  Point  La  Jollo:  U.S.  Geologicol  Survey  Open-File  Report 
75-629,  28  p. 

Moore,  G.W.,  1976,  Hypothetical  late  Cenozoic  development  of  the 
California  borderland  and  adjacent  ports  of  vi-estern  North 
America;  Geological  Society  of  America  Abstracts  with  Pro- 
grams, V.  8,  p.  397. 

Moore,  G.W.,  1976,  Basin  development  in  the  California  borderland 
and  the  Basin  and  Range  province,  in  Howell,  D.G.,  editor. 
Aspects  of  the  geologic  history  of  the  California  continental 
borderland:  American  Association  of  Petroleum  Geologists,  Pa- 
cific Section,  Miscellaneous  Publication  24,  p.  383-391. 

Moore,  G.W.,  and  Beyer,  L.A.,  1975,  Seismic  reflection  profiles,  R/V 
KELEZ,  November-December  1973,  continental  borderland  of 
southern  California:  U.S.  Geological  Survey  Open-File  Report 
75-330,  43  p. 

Moore,  G.W.,  and  Kennedy,  M.P.,  1970,  Coastal  geology  of  the 
Colifornia-Baja  California  border  area,  in  Pacific  slope  geology 
of  northern  Bajo  California  and  odjocent  Alto  California:  Ameri- 
can Association  of  Petroleum  Geologists,  Society  of  Economic 
Paleontologists  and  Mineralogists,  and  Society  of  Exploration 
Geophysicists,  Pacific  Sections,  p.  4-9. 

Moore,  G.W.,  and  Kennedy,  M.P.,  1975,  Quaternary  faults  in  San 
Diego  Bay,  California:  Journal  of  Research,  U.S.  Geological  Sur- 
vey, V.  3,  p.  589-595. 

Moore,  G.W.,  and  Kennedy,  M.P.,  1976,  Acoustic-reflection  profiles, 
Scripps  utility  boat.  Son  Diego  Boy,  California:  U.S.  Geological 
Survey  Open-File  Report  76-562,  9  p. 

Moore,  G.W.,  and  Luken,  M.D.,  1979,  Offshore  sand  and  gravel 
resources  of  the  Pacific  northwest:  Oregon  Geology,  v.  41,  no. 
9,  p.  143-151. 

Moore,  G.W.,  and  McCulloch,  D.S.,  1975,  Acoustic-reflection  pro- 
files, M/V  OIL  CITY,  June  1969,  offshore  southern  California: 
U.S.  Geological  Survey  Open-File  Report  75-347. 

Moore,  G.W.,  and  Silver,  E.A.,  1968,  Geology  of  the  Klamath  River 
delta,  California:  U.S.  Geological  Survey  Professional  Paper 
600-C,  p.  CI 44- 148. 

Moore,  G.W.,  and  Silver,  E.A.,  1968,  Gold  distribution  of  the  sea 
floor  off  the  Klamath  Mountains,  California:  U.S.  Geological 
Survey  Circular  605,  9  p. 

Morner,  N.-A.,  1983,  Comment  on  "Tectonic  uplift  of  a  middle 
Wisconsin  marine  platform  near  the  Mendocino  triple  junction, 
California":  Geology,  v.  11,  p.  621. 

Muhs,  D.R.,  1979,  Marine  terrace  age  assignments,  uplift  rates  and 
sea  level  events  on  Son  Clemente  Island,  California:  Geological 
Society  of  America  Abstracts  with  Programs,  v.  1 1,  no.  7,  p.  484. 

Muhs,  D.R.,  1983,  Quaternary  sea-level  events  on  northern  San 
Clemente  Island,  California:  Quaternary  Research,  v.  20,  p.  322- 
341. 

Muhs,  D.R.,  1985,  Amino  acid  age  estimates  of  marine  terraces  and 
sea  levels  on  Son  Nicolas  Island,  California:  Geology,  v.  13,  p. 
58-61. 

Muhs,  D.R.,  and  Rosholt,  J.N.,  1984,  Ages  of  marine  terraces  on  the 
Polos  Verdes  Hills,  Colifornia,  by  Amino  acid  and  Uranium  trend 
dating:  Geological  Society  of  America  Abstracts  with  Programs, 
V.  16,  no.  6,  p.  603. 

Muhs,  D.R.,  and  Szobo,  B.J.,  1982,  Uranium-series  age  of  the  Eel 
Point  terrace.  Son  Clemente  Island,  California:  Geology,  v.  10, 
p.  23-26. 

Mulhern,  M.E.,  1976,  Physiocochemicol  characterization  of  sediment 
focies  and  poleoclimotic  inferences,  California  continental  bor- 
derland: University  of  Southern  California,  unpublished  Master's 
Thesis. 
Mullins,  H.T.,  and  Nogel,  D.K.,  1981,  Franciscan-type  rocks  off  Mon- 
terey Boy,  California,  implications  for  western  boundary  of 
Solinian  block:  Geo-morine  Letters,  v.  1,  p.  135-139. 


Mullins,  H.T.,  and  Nogel,  D.K.,  1982,  Evidence  for  shallow  hydrocar- 
bons  offshore    northern    Santa    Cruz   County,    California:   The 
American  Association  of  Petroleum  Geologists  Bulletin,  v.  66,  no. 
8,  p.  1055-1075. 
Murphy,.  L.M.,  and  Cloud,  W.K.,  1954,  United  States  earthquakes — 

1952:  U.S.  Coast  Geodetic  Survey  Series  773. 
Murray,  S.M.,  1972,  Diogenesis  of  sediment  in  the  Santo  Barbara 
basin  of  the  California  borderland:  University  of  Southern  Cali- 
fornia unpublished  Master's  Thesis. 
Mutch,  P.,  Lindh,  A.,  Reneou,  D.,  and  McCulloch,  D.,  1986,  Seismicity 
of  the  central  California  coastal  region  from  Point  Buchon  to 
Point  Piedros  Bloncos  for  selected  time  periods  in  1980-1981: 
U.S.  Geological  Survey   (in  press). 
Nogle,  D.  K.,  Mullins,  H.  T.,  and  Greene,  H.  G.,  1986,  Ascension 
Submarine    Canyon,     California — Evolution    of    a    multi-head 
canyon    system  along  a   strike-slip  continental  morgin;  Marine 
Geology,  73,  p.  285-310. 
Nagle,  H.E.,  and  Parker,  E.S.,  1971,  Future  oil  and  gas  potential  of 
onshore  Ventura  basin,  California,  in  Cram,  I.H.,  editor.  Future 
petroleum  provinces  of  the  United  Stotes — their  geology  ond 
potential:  American  Association  of  Petroleum  Geologists  Memoir 
14,  V.  1  p.  254-297. 
Nordin,  T.R.,  1976,  Late  Cenozoic  history  of  the  Santo  Monica  Boy: 
University  of  Southern  Colifornio  unpublished  Master's  Thesis. 
Nordin,  T.R.,  1977,  The  Quaternary  stratigraphy  of  the  Santa  Mon- 
ica and  Son  Pedro  shelves;  California  continental  borderland: 
American  Association  of  Petroleum  Geologists — Society  of  Eco- 
nomic Paleontologists  and  Mineralogists  Annual  Meeting. 
Nordin,  T.R.,   1978,   Geophysical  evidence  for  subaqueous  mass 
movement  in  Santo  Cruz  basin,  California  continental  border- 
land: Geological  Society  of  America  Abstracts  with  Programs,  v. 
10,  p.  462. 
Nordin,  T.R.,   1978,  Hydrocarbon  seepage  in  Santa  Monico  Boy; 
California  continental  borderland:  American  Association  of  Pe- 
troleum Geologists  Bulletin,  v.  62,  p.  548. 
Nardin,  T.R.,  1981,  Seismic  stratigraphy  of  Santo  Monica  and  Son 
Pedro  basins,  California  continental  borderland;  late  Neogene 
history  of  sedimentation  and  tectonics:  University  of  Southern 
California,  unpublished  Doctoral  Thesis. 
Nordin,  T.R.,  Edwords,  B.D.,  and  Gorsline,  D.S.,  1979,  Sonto  Cruz 
basin,  California  borderland;  dominance  of  slope  processes  in 
basin  sedimentation,  in  Doyle,  L.J.  and  Pilkey,  O.H.,  editors. 
Geology  of  continental  slopes:  Society  of  Economic  Paleontolo- 
gists and  Mineralogists  Special  Publication  27,  p.  209-221. 
Nardin,  T.R.,  and  Gorsline,  D.S.,   1981,  Basin  filling  sequences  in 
active  margin  basins  determined  by  seismic  strotigrophic  meth- 
ods, in  Douglas,  R.D.,  Coldburn,  I. P.,  and  Gorsline,  D.S.,  editors, 
Depositional  systems  of  active  margin  basins;  Short  course  notes: 
Pacific  Section  SEPM,  Los  Angeles,  p.  85-98. 
Nardin,  T.R.,  Hein,  F.J.,  Gorsline,  D.S.,  and  Edwards,  B.D.,  1979,  A 
review  of  moss  movement  processes,  sediment  and  acoustic  char- 
acteristics ond  contrasts  in  slope  and  bose-of-slope  systems  ver- 
sus conyon-fon-bosin  floor  systems,  in  Doyle,  L.J.,  and  Pilkey, 
O.H.,  editors.  Geology  of  continental  slopes:  Society  of  Econom- 
ic Paleontologists  and  Minerologists  Special  Publication  27,  p. 
63-77. 
Nardin,  T.R.,  and   Henyey,  T.L.,   1978,   Pliocene-Pleistocene  dios- 
trophism  of  Sonto  Monica  and  Son  Pedro  shelves,  Colifornia 
continental    borderland:    American    Association    of    Petroleum 
Geologists  Bulletin,  v.  62,  p.  247-272. 
Nardin,  T.R.,  and   Henyey,   T.L.,    1978,   Pliocene-Pleistocene  dios- 
trophism  of  Sonto  Monico  ond   Son   Pedro  shelves,  California 
continental  borderland  reply:  American  Associotion  of  Petroleum 
Geologists  Bulletin,  v.  62,  p.  2496-2497. 
Noson,  R.,  1968,  San  Andreas  Fault  at  Cope  Mendocino:  Proceed- 
ings of  Conference  on  Geologic  Problems  of  Son  Andreas  Fault 


98 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


System,  Stanford  University  Publication  in  Geological  Sciences, 
y.  2,  p.  231-241. 

Notlond,  M.L.,  1933,  Temperature  ond  deptti  ranges  of  some  recent 
and  fossil  forominifero  in  the  southern  California  region:  Scripps 
Institution  of  Oceanography  Bulletin,  Technical  Series,  v.  3,  no. 
10. 

Notlond,  M.I.,  and  Kuenen,  P.H.,  1951,  Sedimentary  history  of  the 
Venturo  basin,  Californio:  Society  of  Mineralogists  ond  Paleon- 
tologists Special  Publication  2,  p.  76-107. 

Nelson,  C.H.,  Normork,  W.R.,  Boumo,  A.H.,  and  Carlson,  P.R.,  1976, 
Thin-bedded  turbidiles  in  modern  submarine  canyons  and  fons: 
American  Association  of  Petroleum  Geologists  Bulletin,  v.  60,  p. 
702-703. 

Nelson,  C.H.,  Normork,  W.R.,  Boumo,  A.H.,  and  Carlson,  P.R.,  1978, 
Thin-bedded  turbidites  in  modern  submarine  canyons  and  fans, 
in  Stanley,  D.J.,  and  Kelling,  G.,  editors.  Sedimentation  in  sub- 
marine canyons,  fans,  and  trenches:  Dowden,  Hutchinson,  and 
Ross,  Stroudsburg,  Pennsylvania,  p.  177-189. 

Nelson,  T.W.,  and  Burk,  C.A.,  1966,  Petroleum  resources  of  the 
continental  margins  of  the  United  States,  in  Exploiting  the 
Oceon:  Second  Annual  Conference  of  the  Marine  Technology 
Society  Tronsoctions,  p.   116-133. 

Nilsen,  T.H.,  1980,  Modern  and  ancient  submarine  fans^-discussion 
of  popers  by  R.G.  Walker  ond  W.R.  Normork:  American  Associa- 
tion of  Petroleum  Geologists  Bulletin,  v.  64,  p.  1094-1101. 

Nilsen,  T.H.,  and  Clarke,  S.H.,  Jr.,  1975,  Sedimentation  and  tecton- 
ics in  the  early  Tertiary  continental  borderland  of  central  Califor- 
nia: U.S.  Geological  Society  Professional  Paper  925,  64  p. 

Nilsen,  T.H.,  Taylor,  F.A.,  and  Dean,  R.M.,  1976/1977,  Natural 
conditions  that  control  londsliding  in  the  San  Francisco  Boy  re- 
gion— on  analysis  based  on  doto  from  the  1968-1969  and  1972- 
1973  roiny  seasons:  U.S.  Geological  Survey  Bulletin  1424,  p.  35. 

Noble,  F.J.,  1966,  Huntington  Beach  offshore — Parcel  14:  American 
Association  of  Petroleum  Geologists  Bulletin,  v.  50,  p.  649. 

Nocito,  B.W.,  1977,  Cloy-siie  C0CO3  ond  cloy  mineralogy  of  recent 
marine  sediments;  southern  California  borderland:  University  of 
California,  Son  Diego,  unpublished  Master's  Thesis. 

Nolf,  B.,  and  Nolf,  P.,  1969,  Santo  Cruz  Island  voiconics,  in  Weaver, 
D.W.,  and  others,  editors.  Geology  of  the  northern  Channel 
Islands:  American  Association  of  Petroleum  Geologists  and  Soci- 
ety of  Economic  Paleontologists  and  Mineralogists,  Pacific  Sec- 
tions, Speciol  Publicotion,  p.  91-94. 

Nordquist,  J.M.,  1964,  A  catalog  of  southern  California  earth- 
quakes, and  associated  electronic  data  processing  programs: 
Seismologicol  Society  of  America  Bulletin,  v.  54,  p.  1003-1011. 

Nordstrom,  C.E.,  and  Morgolis,  S.V.,  1972,  Sedimentary  history  of 
central  California  shelf  sands  as  revealed  by  scanning  electron 
microscopy:  University  of  California,  San  Diego,  Scripps  Institu- 
tion of  Oceonogrophy,  Contributions,  v.  42,  p.  902-911. 

Normork,  W.R.,  1969,  Growth  patterns  of  deep  seo  fons:  Marine 
Physical  Loboratory  of  the  Scripps  Institution  of  Oceanography, 
SIO  Reference  69-29,  77  p. 

Normork,  W.R.,  1978,  Fon  valleys,  channels,  and  deposltlonal  lobes 
on  modern  submarine  fans:  characters  for  recognition  of  sandy 
turbldlte  environments:  American  Association  of  Petroleum 
Geologists  Bulletin,  v.  62,  no.  6,  p.  912-931. 

Normork,  W  R.,  1970,  Channel  piracy  on  Monterey  deep-sea  fon: 
Deep  Sea  Research,  v.   17,  p.  837-846. 

Normork,  W  R  ,  1970.  Growth  patterns  on  deep  sea  fans:  American 
Associolion  of  Petroleum  Geologists  Bulletin,  v.  54,  p.  2170- 
2195. 

Normork,  W.R.,  1974,  Submarine  canyons  and  fan  volleys:  factors 
affecting  growth  patterns  of  deep-sea  fans,  in  Doft,  R.H.,  Jr.,  and 
Shaver,  R.H.,  Modern  ond  ancient  geo-synclinol  sedimentation: 
SEPM  Special  Publlcalion  19,  p.  56-68. 


Normork,  W.R.,  1980,  Modern  ond  ancient  submarine  fans.  Reply: 
American  Association  of  Petroleum  Geologists  Bulletin,  v.  64,  p. 
1108-1112. 

Normork,  W.R.,  Alpha,  T.R.,  and  Hess,  G.R.,  1980,  Geomorphic 
features  of  the  Navy  submarine  fan,  California  continental  bor- 
deriond:  U.S.  Geologlcol  Survey  Field  Studies  Mop  MF-1135. 

Normork,  W.R.,  Ford,  G.A.,  and  Chose,  T.E.,  1980,  Trockline  mop 
and  acoustic  profiles  showing  deep-tow  geophysicol  doto  from 
the  northern  segment  of  the  Son  Clemente  fault,  California  bor- 
derland: U.S.  Geologicol  Survey  Open-File  Report  80-932,  2 
sheets. 

Normork,  W.R.,  Gutmocher,  C.E.,  1983/1984,  Delgado  fan;  prelimi- 
nary interpretation  of  channel  development:  Geo-Morlne  Letters, 
V.  3,  p.  79-83. 

Normork,  W.R.,  Gutmocher,  C.E.,  Chose,  T.E.,  ond  Wilde,  P.,  1983/ 
1984,  Monterey  fan;  growth  pattern  controlled  by  basin  mor- 
phology and  changing  sea  levels:  Geo-Morlne  Letters,  v.  3,  p. 
93-99. 

Normork,  W.R.,  and  Hess,  G.R.,  1978,  Sedimentologicol  features 
and  growth  of  the  Monterey  deep-sea  fan  off  central  California: 
U.S.  Geological  Survey  Professionol  Paper  1100,  p.  151. 

Normork,  W.R.,  and  Hess,  G.R.,  1980,  Quaternary  growth  patterns 
of  California  submarine  fans,  in  Field,  M.E.,  Boumo,  AH.,  Col- 
burn,  I.,  Douglas,  R.G.,  and  Ingle,  J.C.,  editors,  Quotemory 
deposltlonal  environments  of  the  Pacific  coast:  Pacific  Coast 
Poleogeogrophy  Symposium,  Port  4,  Poclfic  Section  Society  Eco- 
nomic Paleontologists  and  Mineralogists,  p.  201-210. 

Normork,  W.R.,  Hess,  G.R.,  Chose,  T.E.,  Wilde,  P.,  and  Spencer, 
T.E.,  1977,  Active  and  relict  channel  systems  ond  growth  pattern 
on  Monterey  fan,  California:  Geological  Society  of  Americo  Ab- 
strocts  with  Programs,  v.  9,  p.  116. 

Normork,  W.R.,  Hess,  G.R.,  and  Spiess,  F.N.,  1978,  Mapping  of 
small  scale  (outcrop-size)  sedimentologicol  feotures  on  modem 
submarine  fons:  Offshore  Technology  Conference,  Tenth,  no. 
3120,  p.  593-598. 

Normork,  W.R.,  Hess,  G.R.,  Stow,  D.A.V.,  and  Bowen,  A.J.,  1980, 
Sediment  waves  on  the  Monterey  fon  levee;  a  preliminary  physi- 
cal interpretation:  Marine  Geology,  v.  37,  p.   1-18. 

Normork,  W.R.,  Loughridge,  M.S.,  and  Spiess,  F.N.,  1968,  Detailed 
channel  morphology  of  the  La  Jolla  submarine  fan  volley:  Ameri- 
con  Geophysical  Union  Transactions,  v.  49,  p.  212. 

Normork,  W.R.,  ond  Piper,  D.J.W.,  1969,  Deep-seo  fan  volleys,  post 
and  present:  Geological  Society  of  America  Bulletin,  v.  80,  p. 
1859-1866. 

Normork,  W.R.,  and  Piper,  D.J.W.,  1972,  Sediments  and  growth 
pottern  (at)  of  Novy  deep-seo  fan.  Son  Clemente  basin,  Califor- 
nia borderland:  Scripps  Institution  of  Oceonogrophy  Contribu- 
tions, V.  42,  p.   1094-1119. 

Normork,  W.R.,  ond  Piper,  D.J.W.,  1972.  Sediments  and  growtti 
pattern  of  Novy  deep-sea  fan.  Son  Clemente  basin,  California 
borderland:  Journal  of  Geology,  v.  80,  p.   198-223. 

Normork,  W.R.,  and  Piper,  D.J.W.,  1983  1984,  Novy  fan,  California 
borderland:  growth  pottern  ond  deposltlonal  processes:  Geo- 
Morine  Letters,  v.  3,  p.   101   108. 

Normork,  W.R.,  Piper,  D.J.W.,  and  Hess,  G.R.,  1979,  Distributary 
channels,  sand  lobes,  and  mesolopogrophy  of  Novy  submarine 
fan,  California  borderland,  with  applications  to  ancient  fan  sedi- 
ments: Sedlmenlology,  v    26,  p.  749-774. 

Norris,  R.M.,  1951,  Morine  geology  of  the  Son  NIcolos  Island  region, 
California:  Scripps  Institution  of  Oceonogrophy  unpublished 
Doclorol  Thesis. 

Norris,  R.M.,  1951,  Marine  geology  of  the  Son  Nicolas  Islond  region, 
Californio:  Scripps  Institution  of  Oceonogrophy,  Submarine  Ge- 
ology Report  21,  14  p. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


99 


Norris,  R.M.,  1952,  Recent  history  of  a  sand  spit  at  San  Nicolas 
Island,  California:  Journol  of  Sedimentary  Fetology,  v.  22,  p. 
224-228. 

Norris,  R.M.,  1964,  Dams  and  beach-sand  supply  in  southern  Califor- 
nia, in  Miller,  R.L.,  editor.  Papers  in  Marine  Geology,  Shepard 
Commemorative  Volume:  Mocmillan,  New  York,  NY,  p.  154-171. 

Northrop,  J.,  Menard,  H.W.,  and  Duennebier,  F.K.,  1968,  Seismic 
and  both/metric  evidence  of  a  fracture  zone  on  the  Gordo  Ridge: 
Science,  v.  161,  p.  688. 

Nowroozi,  A. A.,  1973,  Seismicity  of  the  Mendocino  Escarpment  and 
the  aftershock  sequence  of  June  26,  1968,  ocean  bottom  seismic 
measurements:  Seismologicol  Society  of  America  Bulletin,  v.  63, 
p.  441-456. 

Nowroozi,  A. A.,  Ewing,  M.,  Nafe,  J.,  and  Fliegel,  M.,  1968,  Deep 
ocean  current  and  its  correlation  with  the  ocean  tide  off  the  coast 
of  northern  California:  Journal  of  Geophysical  Research,  v.  73, 
p.  1921-1932. 

O'Day,  M.S.,  1974,  The  structure  and  petrology  of  the  Mesozoic  and 
Cenozoic  rocks  of  the  Franciscan  Complex,  Leggett-Piercy  area, 
northern  California  Coast  Ranges:  Davis,  California,  University  of 
California  unpublished  Doctoral  Thesis,  152  p. 

Ogle,  B.A.,  1953,  Geology  of  the  Eel  River  Valley  area,  Humboldt 
County,  California:  California  Division  of  Mines  and  Geology 
Bulletin  164,  128  p. 

Olmstead,  F.H.,  1958,  Geological  reconnaissance  of  San  Clemente 
Island,  California:  U.S.  Geologicol  Survey  Bulletin  1071-B,  p. 
B55-B68. 

O'Neil,  T.J.,  1976,  Source  identification  of  beach  tars  within  south- 
ern California  borderland:  American  Association  of  Petroleum 
Geologists  Bulletin,  v.  60,  p.  704. 

Orlin,  H.,  Jones,  R.B.,  Fanning,  K.F.,  and  Goroutte,  S..K.,  1962,  Sea 
gravity  phase,  oceonographic  equipment  evaluation  range,  San 
Francisco,  California::  U.S.  Coast  and  Geodetic  Survey  and  U.S. 
Naval  Oceonographic  Office  Report,  24  p.  2  mops,  scale  1:200,- 
000. 

Orr,  P.C,  1956,  Radiocarbon  dates  from  Santa  Rosa  Island,  I:  Santa 
Barbara  Museum  of  Natural  History  Bulletin,  v.  2,  10  p. 

Orr,  P.C,  1959,  Lower  Pleistocene  marine  terraces  on  Santa  Rosa 
Island,  California:  Geological  Society  of  America  Bulletin,  v.  70, 
p.  1738-1739. 

Orr,  P.C,  1960,  Late  Pleistocene  marine  terraces  on  Santa  Rosa 
Island,  California:  Geological  Society  of  America  Bulletin,  v.  71, 
p.  1113-1119. 

Orr,  P.C,  1960,  Radiocarbon  dotes  from  Santa  Rosa  Island,  II:  Santa 
Barbara  Museum  of  Natural  History  Bulletin,  v.  3,  9  p. 

Orr,  P.C,  1968,  Prehistory  of  Santo  Rosa  Island,  Santo  Barbara, 
California,  Santo  Barbara  Museum  of  Natural  History  Bulletin, 
253  p. 

Orr,  P.C,  Broecker,  W.S.,  1957,  Sea-level  changes  on  Santo  Rosa 
Island,  Colifornio:  Geological  Society  of  America  Bulletin,  v.  68, 
p.  1840. 

Orr,  W.L.,  and  Emery,  K.O.,  1956,  Composition  of  organic  matter 
in  marine  sediments — preliminary  data  on  hydrocarbon  distribu- 
tion in  basins  off  southern  California:  Geological  Society  of 
America  Bulletin,  v.  67,  p.  1247-1258. 

Orr,  W.L.,  Emery,  K.O.,  and  Grady,  J.R.,  1958,  Preservation  of 
chlorophyll  derivatives  in  sediments  of  southern  California: 
American  Association  of  Petroleum  Geologists  Bulletin,  v.  42,  p. 
925-962. 

Orr,  W.L.,  and  Grady,  J.R.,  1967,  Perylene  in  basin  sediments  off 
southern  California:  Geochimico  et  Cosmochimico  Acta,  v,  31,  p. 
1201-1209. 

Osborne,  R.H.,  Scheidemonn,  R.C,  Jr.,  Nordin,  T.R.,  and  Harper, 
A.S..,  1980,  Quaternary  stratigraphy  and  depositionol  environ- 
ments, Santo  Monica  Bay,  southern  California,  in  Field,  M.E., 
Bouma,  A.H.,  Douglas,  R.G.,  and  Ingle,  J.C,  editors.  Quaternary 


depositionol  environments  of  the  Pacific  Coast:  Society  of  Eco- 
nomic Paleontologists  and  Mineralogists,  Pacific  Section,  Pacific 
Coast  Poleogeogrophic  Symposium  4,  p.  143-156. 

Page,  B.M.,  1970,  Sur-Nocimiento  fault  zone  of  California:  Conti- 
nental margin  tectonics:  Geological  Society  of  America  Bulletin, 
V.  81,  p.  667-690. 

Page,  B.M.,  and  Engebretson,  D.C,  1984,  Correlation  between  the 
geologic  record  and  computed  plate  motions  for  central  Califor- 
nia: Tectonics,  v.  3,  no.  2,  p.  133-155. 

Page,  B.M.,  Wagner,  H.C,  McCulloch,  D.S.,  Silver,  E.A.,  and  Spotts, 
J.O.,  1979,  Geologic  cross  section  of  the  continental  margin  off 
San  Luis  Obispo,  the  southern  Coast  Ranges,  and  the  Son  Joa- 
quin Valley,  California:  Geological  Society  of  America  Mop 
Chart  Series  MS-28G,  12  p. 

Page,  B.M.,  Wagner,  H.C,  McCulloch,  D.S.,  Silver,  E.A.,  and  Spotts, 
J.O.,  1979,  Tectonic  interpretation  of  a  geologic  section  of  the 
continental  margin  off  San  Luis  Obispo,  the  southern  Coast 
Ranges,  and  the  San  Joaquin  Valley,  California — cross  section 
summary:  Geological  Society  of  America  Bulletin,  v.  90,  p.  808- 
812. 

Palmer,  H.D.,  1964,  Marine  geology  of  Rodriguez  Seamount:  Deep- 
Seo  Research,  v.  11,  p.  737-756. 

Palmer,  H.D.,  1965,  Geologic  significance  of  Davis  Seoknoll,  Arguel- 
lo  Plateau,  California:  Geological  Society  of  America  Bulletin,  v. 
76,  p.  379-384. 

Palmer,  H.D.,  1965,  Geology  of  Richardson  Rock,  northern  Channel 
Islands,  Santo  Barbara  County,  California:  Geological  Society  of 
America  Bulletin,  v.  76,  p.  1197-1202. 

Palmer,  H.D.,  1965,  Submarine  geography  of  southern  California: 
Journal  of  the  West,  v.  4,  p.  77-94. 

Palmer,  H.D.,  1971,  Observations  on  the  erosion  of  submarine  out- 
crops. La  Jolla  submarine  canyon,  California:  Geological  Society 
of  America  Abstracts  with  Programs,  v.  3,  p.  666. 

Palmer,  H.D.,  Scholl,  D.W.,  and  Green,  J.,  1965,  A  peculiar  pedesta- 
lote  terrace,  San  Nicolas  Island,  California:  Journal  of  Sedimen- 
tary Petrology,  v.  35,  p.  507-511. 

Pompeyon,  E.H.,  1979,  Preliminary  map  showing  recency  of  faulting 
in  coastal  north-central  California:  U.S.  Geological  Survey  Mis- 
cellaneous Field  Studies,  MF-1070. 

Pao,  G.A.,  1977,  Sedimentary  history  of  California  continental  bor- 
derland basins  as  indicated  by  organic  carbon  content:  Univer- 
sity of  Southern  California,  unpublished  Master's  Thesis. 

Parker,  F.S.,  1965,  Summary  geology  of  offshore  oil  producing  and 
potential  areas  off  Pacific  coast:  American  Association  of  Petro- 
leum Geologists  Bulletin,  v.  49,  p.  1087-1088. 

Parker,  F.S.,  1971,  Petroleum  potential  of  southern  California  off- 
shore, in  Future  petroleum  provinces  of  the  United  States — their 
geology  and  potential:  American  Association  of  Petroleum 
Geologists  Memoir  15,  p.  178-191. 

Patterson,  R.H.,  1979,  Tectonic  geomorphology  and  neotectonics  of 
the  Sonto  Cruz  Island  fault,  Santo  Barbara  County,  California: 
University  of  California,  Sonto  Barbara,  unpublished  Doctoral 
Thesis,  140  p. 

Paul,  R.C,  Arnol,  R.E.,  Boysinger,  J. P.,  Cloypool,  G.E.,  Holte,  J.L., 
Lubeck,  CM.,  Potterson,  J.M.,  Moore,  R.Z.  Sletene,  R.L.,  Sliter, 
W.V.,  Toylor,  J.C,  Tudor,  R.B.,  and  Webster,  F.L.,  1976,  Geologi- 
cal and  operational  summary,  southern  California  deep  stroti- 
grophic  test  OCS-CAL  75-70  no.  1,  Cortes  Bonk  area  offshore 
California:  U.S.  Geological  Survey  Open-File  Report  76-232,  65 

P- 
Payne,  CM.,  Schell,  B.A.,  and  Swonson,  D.E.,   1979,  Quaternary 
faulting   in   the   offshore   region   between   Point   Sol   and    Point 
Conception,  Cqlifornio:  Geological  Society  of  America  Abstracts 
with  Progroms,  v.  11,  p.  121. 


100 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


Payne,  CM.,  Swanson,  D.E.,  and  Schell,  B.A.,  1978,  Investigation 
of  the  Hosgri  foult  offshore  southern  California,  Point  Sol  to  Point 
Conception:  U.S.  Geological  Sunrey  Open-File  Report  79-1199. 

Poyton,  C.W.,  1977,  Seismic  stratigraphy — applications  to  hydro- 
carbon exploration:  American  Association  of  Petroleum  Geolo 
gists.  Memoir  26,  516  p. 

Peterson,  D.H.,  McCulloch,  D.S.,  Conomos,  T.J.,  and  Carlson,  P.R., 
1972,  Distribution  of  lead  and  copper  in  surface  sediments  in  the 
San  Francisco  Boy  estuory,  California:  U.S.  Geological  Survey 
Miscellaneous  Field  Studies,  MF-323 

Phillips,  R.L.,  1979,  Heavy  minerals  and  bedrock  minerals  on  the 
continental  shelf  of  Washington,  Oregon,  and  California:  U.S. 
Department  of  Commerce,  Springfield,  Virginia,  National  Techni- 
cal Information  Service  Publication  Number  81-192601.  56  p. 

Pierce,  J.W.,  and  Melson,  W.G.,  1967,  Dolomite  from  the  continen- 
tal slope  off  southern  California:  Journal  of  Sedimentary  Petrol- 
ogy, V.  37,  p.  962-966. 

Pilger,  R.H.,  Jr.,  1976,  Structure  of  Santa  Cruz  -  Catalina  Ridge  and 
adjacent  areas,  southern  California  continental  borderland,  from 
reflection  and  magnetic  profiling;  implications  for  late  Cenozoic 
tectonics  of  southern  California:  University  of  Southern  Califor- 
nia, unpublished  Doctoral  Thesis. 

Pilger,  R.H.,  Jr.,  1976,  Structure  of  Santa  Cruz-Catalino  Ridge,  Cali- 
fornia borderland;  implications  for  the  Neogene  tectonics  of 
southern  California:  American  Geophysical  Union  Transactions, 
V.  59,  p.  1211. 

Pilger,  R.H.,  Jr.,  Henyey,  T.L.,  1977,  Plate  tectonic  reconstructions 
and  the  Neogene  tectonic  and  volcanic  evolution  of  the  Califor- 
nia borderland  and  Coast  Ranges:  Geological  Society  of  Ameri- 
ca Abstracts  with  Programs,  v.  9,  p.  482. 

Pilger,  R.H.,  Jr.,  Henyey,  T.L.,  1978,  Pacific-North  American  plate 
interaction  and  Neogene  volcanism  in  coastal  California:  Tec- 
tonophysics,  v.  57,  p.  189-209. 

Pilkey,  OH.,  Locker,  S.C,  and  Cleary,  W.J.,  1980,  Comparison  of 
sandlayer  geometry  on  flat  floors  of  ten  modern  depositional 
basins:  American  Association  of  Petroleum  Geologists  Bulletin,  v. 
64,  p.  841-856. 

Piper,  D.J.W.,  1970,  Transport  and  deposition  of  Holocene  sediment 
on  La  Jollo  deep-sea  fan,  California:  Marine  Geology,  v.  8,  p. 
211  227. 

Piper,  D.J.W.,  1971,  Lower  Copistrano  formation  at  Dona  Harbor; 
notes  on  turbidite  sedimentology,  in  Geologic  Guidebook,  New- 
port Lagoon  to  Son  Clemente,  Orange  County,  Coiifornio:  Soci- 
ety of  Economic  Paleontologists  and  Mineralogists,  Pacific 
Section,  p.  37-40. 

Piper,  D.J.W.,  and  Marshall,  N.F.,  1969,  Bioturbation  of  Holocene 
sediments  on  La  Jollo  deep-sea  fan,  California:  Journal  of  Sedi 
mentory  Petrology,  v.  39,  p.  601606. 

Piper,  D.J.W.,  and  Normork,  W.R.,  1971,  Reexamination  of  a  Mio- 
cene deep-sea  fan  and  fan-valley,  southern  California:  Geologi- 
cal Society  of  America  Bulletin,  v.  82,  p.   1823-1830. 

Piper,  D.J.W.,  and  Normark,  W.R.,  1983,  Turbidite  depositional 
pattern  ond  flow  characteristics.  Navy  submarine  fan,  Coiifornio 
Borderland,  Sedimentology,  v.  30,  p.  681-694. 

Piper,  D.J.W  ,  Normark,  W.R.,  and  Ingle,  J.C,  Jr.,  1976,  The  Rio  Dell 
Formation:  a  Plio-Pleistocene  basin  slope  deposit  in  northern 
California:  Sedimentology,  v.  23,  p    309-328. 

Piper,  D.Z.,  and  Fowler,  B.,  1979,  Sediment  chemistry,  in  Cook  H.E  , 
editor.  Geologic  studies  of  the  Point  Conception  deep  strati 
graphic  test  well:  U.S.  Geological  Survey  Open-File  Report  79- 
1218,  p   97  108. 

Pipkin,  B.W.,  1979,  Southern  California  continental  borderland  and 
extraction  of  natural  resources,  in  Friedheim,  R.L.,  editor,  Monog 
ing  ocean  resources;  o  primer:  Westview  Press,  p.  45-50 

Pipkin,  6.W.,  Hunt,  G.S.,  Kolpock,  R.L,  and  Slosson.  J  E.,  1973, 
Geologic  Guidebook,  Catalina  Island  ond  continenlol  border- 


land of  southern  Coiifornio:  Association  of  Engineering  Geolo- 
gists Annual  Meeting,  1973. 
Pipkin,    B.W.,    Ribi,    H.L.,    Kelejion,    J.,    and    Salmons,    J.E.,    1967, 
Progress  report  on  study  of  beach  nourishment  along  the  southern 
Coiifornio  coastline:  California  Department  of  Water  Resources 
Report,  59  p. 
Pirie,  DM.,  and  Stellar,  D.G.,  1977,  California  coastal  processes — 
LANDSAT  II,  Final  Report:  Notional  Aeronautics  and  Spoce  Ad- 
ministration Goddord  Space  Flight  Center,  Greenbelt,  Marylond, 
146  p. 
Pisios,  N.G.,  1978,  Paleoceonogrophy  of  the  Sonto  Barbara  basin 
during  the  last  8,000  years:  Quaternary  Research,  p.  366-384. 
Pisios,  N.G.,  1979,  Model  for  poleoceanogrophic  reconstructions  of 
the  California  current  during  the  lost  8,000  years:  Quaternary 
Research,  v.  11,  p.  373-386. 
Pitman,  W.C,  III,  Larson,  R.L.,  and  Herron,  E.M.,  1974,  The  age  of 
the  ocean  basins:  Geological  Society  of  America  Mop  and  Chart 
Series,  no.  6,  4  p. 
Pollard,  D.D.,  1979,  The  source  ond  distribution  of  beach  sediments, 
Sonto    Barbara    County,    California:    University    of    California, 
Santa  Barbara,  unpublished  Doctoral  Thesis. 
Piatt,  J. P.,  1972,  Cotolino  Schist,  Sonto  Catalina  Island,  Coiifornio: 
Geological  Society  of  America  Abstracts  with  Programs,  v.  4,  p. 
219. 
Piatt,  J. P.,  1976,  The  petrology,  structure,  and  geologic  history  of  the 
Cotolino  Schist  terroin,  southern  Coiifornio:  California  University 
Publicotion  in  Geological  Sciences,  v.  112,  111  p. 
Plott,  J. P.,  1976,  The  significance  of  the  Catalina  Schist  in  the  history 
of  the  southern  California  borderlond,  in  Howell,  D.G.,  editor, 
Aspects   of   the   geologic   history   of   the   California   continental 
borderland:  American  Association  of  Petroleum  Geologists,  Pa- 
cific Section,  Special  Publication  24,  p.  47-52, 
Polski,  W.,  1957,  Varied  sediments  in  a  core  from  the  Santa  Barbara 
basin  off  the  California  coast:  University  of  Southern  California 
unpublished  report,  15  p. 
Prohl,  N.A.,  and  Mills,  G.B.,  1971,  Operational  data  report.  West 
Coast  continental  shelf  bottom  gravity.  Cope  Flottery  to  Sonto 
Cruz,  NOAA  ship  McArthur:  NOAA,  NOS,  Marine  Geophysics 
Group  Report,  50  p. 
Pratt,  W.L.,  Jr.,  1956,  Glouconite  casts  in  some  bottom  sediments 
from   Sonto  Monica  Boy  and  Santa  Roso  Ridge  of<  southern 
Coiifornio:  University  of  Southern  California,  unpublished  report, 
19  p. 
Pratt,  W.L.,  Jr.,  1962,  The  origin  and  distribution  of  glouconite  from 
the  sea  floor  off  California  and  Bojo  California:  University  of 
Southern  California,  unpublished  Doctoral  Thesis. 

Pratt,  W.L.,  Jr.,  1963,  Glouconite  from  the  sea  floor  off  southern 
California,  in  Clements,  T.,  editor.  Essays  in  marine  geology  in 
honor  of  K.O.  Emery:  University  of  Southern  California  Press,  p. 
97- 119. 

Prensky,  S.E.,  1973,  Climatic  and  tectonic  events  recorded  in  late 
Pleistocene  Holocene  deep-sea  sediments,  Coiifornio  border- 
land: Geological  Society  of  America  Abstracts  with  Programs,  v. 
5,  p.  92. 

Raff,  A.D.,  1962,  Further  magnetic  measurements  along  the  Murray 
fault:  Journal  of  Geophysical  reseorch,  v.  67,  p.  417-418. 

Roff,  A.D.,  and  Mason.  R.G  ,  1961,  Magnetic  survey  off  the  west 
coast  of  North  Americo,  40  degrees  N  latitude  to  52  degrees  N. 
latitude:  Geological  Society  of  America  Bulletin,  v.  72,  p.  1267. 

Roitt,  R.W.,  1949,  Studies  of  oceon  bottom  structure  oH  southern 
Coiifornio  with  explosive  waves:  Geological  Society  of  Americo 
Bulletin,  V    60,  p.  1915 

Roitt,  R.W.,  1963,  Seismic  refroction  studies  of  the  Mendocino  frac- 
ture zone:  International  Association  of  Physicol  Oceanography 
Abstracts,   13th  Generol  Assembly,  Berkeley,  v.  6,  p.  71. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


101 


Rand,  W.W.,  1931,  Preliminary  reporf  of  the  geology  of  Santa  Cruz 
Island,  Santo  Barbara  County,  California,  in  Mining  in  California: 
California  State  Mineralogist  Report,  v.  27,  p.  214-219. 

Rond,  W.W.,  1933,  The  geology  of  Santa  Cruz  Island,  California: 
University  of  California,  Berkeley,  unpublished  Doctoral  Thesis. 

Rond,  W.W.,  1951,  Ventura  basin,  in  Possible  future  petroleum 
provinces  of  North  America:  American  Association  of  Petroleum 
Geologists  Bulletin,  v.  35,  p.  231-240. 

Roppeport,  M.L.,  1976,  Holocene  sedimentation  patterns  on  the 
continental  shelf  near  Monterey  Bay,  California,  as  determined 
by  multivariate  analysis  of  heavy  mineral  point  count  data,  in 
Fristche,  A.E.,  TerBest,  H.,  and  Wornordt,  W.W.,  editors.  The 
Neogene  Symposium:  Pacific  Section,  SEPM,  San  Francisco,  p. 
75-84. 

Roppeport,  M.L.,  1976,  Holocene  sedimentation  patterns  deter- 
mined by  multivariate  statistical  analysis  of  heavy  mineral  data, 
Monterey  Bay,  California:  American  Association  of  Petroleum 
Geologists  Bulletin,  v.  60,  p.  2188. 

Real,  C.R.,  Toppozoda,  T.R.,  and  Parke,  D.L.,  1978,  Earthquake 
catalog  of  California — January  1,  1900  to  December  31,  1974: 
California  Division  of  Mines  and  Geology  Special  Publication  52, 
15  p. 

Reed,  R.D.,  1933,  Geology  of  California:  American  Association  of 
Petroleum  Geologists,  355  p. 

Reed,  R.D.,  and  Hollister,  J.S.,  1936,  Structural  evolution  of  southern 
California:  American  Association  of  Petroleum  Geologists,  Tulsa, 
Oklahoma,  157  p. 

Reed,  W.E.,  and  Kaplan,  I.R.,  1977,  The  chemistry  of  marine  petro- 
leum seeps:  Journal  of  Geochemical  Exploration,  v.  7,  p.  255- 
293. 

Rees,  A. I.,  von  Rod,  U.,  and  Shepard,  F.P.,  1968,  Magnetic  fabric 
of  sediments  from  the  La  Jollo  submarine  canyon  and  fan,  Cali- 
fornia: Marine  Geology,  v.  6,  p.  145-178. 

Reinhort,  P.W.,  1970,  Oil  seepage  potentialities  of  Dos  Cuadros  oil 
field,  Santa  Barbara  County,  California:  Santo  Barbara,  Califor- 
nia Environmental  Quality  Advisory  Board  Special  Report,  27  p. 

Resig,  J.M.,  1958,  Ecology  of  foraminifero  of  Santo  Cruz  Basin, 
California:  Micropaleontology,  v.  4,  p.  287-308. 

Revelle,  R.,  and  Shepard,  F.P.,  1939,  Sediments  off  the  California 
coast,  in  Trask,  P.D.,  editor.  Recent  marine  sediments:  American 
Association  of  Petroleum  Geologists,  p.  245-282. 

Rice,  R.M.,  Gorsline,  D.S.,  and  Osborne,  R.H.,  1976,  Relationships 
between  sand  input  from  rivers  and  the  composition  of  sands 
from  the  beaches  of  southern  California:  Sedimentology,  v.  23, 
p.  689-703. 

Richmond,  W.C,  and  Burdick,  D.J.,  1981,  Geologic  hazards  and 
constraints  of  offshore  northern  and  central  California:  13th  An- 
nual Offshore  Technology  Conference,  Houston,  Texas,  OTC 
4117,  p.  9-17. 

Richmond,  W.C,  Burdick,  D.J.,  Phillips,  D.,  and  Norris,  P.J.,  1981, 
Regional  geology,  seismicity,  and  potential  geologic  hazards  and 
constraints,  OCS  oil  and  gas  Lease  Sale  53:  U.S.  Geological 
Survey  Open-File  Report  81-318. 

Richmond,  W.C,  Cummings,  L.J.,  Hamlin,  S.,  and  Nogaty,  M.E., 
1981,  Geological  hazards  and  constraints  in  the  area  of 
proposed  OCS  oil  and  gas  Lease  Sale  48,  southern  California: 
U.S.  Geological  Survey  Open-File  Report  81-307. 

Riddihough,  R.P.,  1980,  Gordo  Plate  motions  from  magnetic  anom- 
aly analysis:  Earth  and  Planetary  Science  Letters,  v.  51,  p.  163- 
170. 

Ridlon,  J.B.,  1968,  Detailed  survey  off  Eel  and  Los  Points  area,  in 
Son  Clemente  Island  rocksite — offshore  geology:  Novol  Weap- 
ons Center  Technical  Publication  4442,  79  p. 

Ridlon,  J.B.,  1969,  Son  Clemente  Island  rocksite  project — offshore 
geology,  reconnaissance  survey  around  the  Island:  National  Un- 


dersea Research  and  Development  Center  Technical  Publication 
156,  130  p. 

Ridlon,  J.B.,  1970,  Bathymetry  and  structure  of  San  Clemente  Island, 
California,  and  tectonic  implications  for  the  southern  California 
continental  borderland:  Oregon  State  University,  unpublished 
Doctoral  Dissertation. 

Ridlon,  J.B.,  1970,  Bathymetry  and  structure  of  Son  Clemente  Island, 
California,  and  tectonic  implications  for  the  southern  California 
borderland:  Oregon  State  University,  unpublished  Doctoral  The- 
sis, 246  p. 

Ridlon,  J.B.,  1972,  Pleistocene-Holocene  deformation  of  the  Son 
Clemente  Island  crustal  block,  California:  Geological  Society  of 
America  Bulletin,  v.  83,  p.  1831-1844. 

Rietmon,  J.D.,  and  Aldrich,  J.K.,  1969,  Gravity  survey  of  the  northern 
Channel  Islands,  in  Weaver,  D.W,,  and  others,  editors.  Geology 
of  the  northern  Channel  Islands,  southern  California  borderland: 
American  Association  of  Petroleum  Geologists  and  Society  of 
Economic  Paleontologists  and  Mineralogists,  Pacific  Sections,  p. 
109-114. 

Rinehart,  V.J.,  1964,  Investigation  of  twelve  earthquakes  off  the 
Oregon  and  northern  California  coasts:  Oregon  State  University, 
unpublished  Master's  Thesis. 

Rintoul,  B.,  1978,  California  offshore:  Pacific  Oil  World,  v.  71,  p. 
94-104. 

Rintoul,  W..T.,  1969,  Deep  oil  revives  Santa  Barbara:  Offshore,  v. 
29,  p.  37-40. 

Rintoul,  W.T.,  1973,  West  coast  offshore:  Oil  World,  Annual  Review, 
p.  74-85. 

Ritter,  W.E.,  1901,  Some  observations  bearing  on  the  probable 
subsidence  during  recent  geological  times  of  the  Island  of  Sonto 
Cotolina  off  the  coast  of  southern  Coifornia:  Science,  v.  14,  p. 
575-577. 

Ritter,  W.E.,  1902,  A  summer's  dredging  on  the  coast  of  southern 
California:  Science,  v.  15,  p.  55-65.  Roberts,  A.E.,  1975,  Selected 
geologic  literature  on  the  California  continental  borderland  and 
adjacent  areas,  to  January  1,  1975:  U.S.  Geological  Survey 
Circular  714,  1 16  p. 

Rodolfo,  K.S.,  1964,  Suspended  sediment  in  southern  California 
waters:  University  of  Southern  California,  unpublished  Master's 
Thesis. 

Rodolfo,  K.S.,  1970,  Annual  suspended  sediment  supplied  to  the 
California  continental  borderland  by  the  southern  California  wa- 
tershed: Journal  of  Sedimentary  Petrology,  v.  40,  p.  666-671. 

Roig,  J.,  1975,  Use  of  heavy  minerals  as  tracers  of  sand  transport 
on  the  Santo  Borbaro-Oxnord  shelf:  Sonto  Barbara,  Colifornio: 
University  of  Southern  California,  unpublished  Master's  Thesis. 

Ross,  A.,  and  Dowlen,  R.J.,  1973,  editors.  Studies  on  the  geology, 
and  geologic  hazards  of  the  greater  Son  Diego  area,  California: 
San  Diego  Association  of  Geologists,  152  p. 

Ross,  D.C,  and  McCulloch,  D.S.,  1979,  Cross  section  of  the  southern 
Coast  Ranges  and  Son  Joaquin  Valley  from  offshore  Point  Sur 
to  Madera,  California:  Geological  Society  of  America  Map  and 
Chart  Series  MC-2,  1  sheet. 

Rothwell,  W.T.,  Jr.,  1958,  Western  Los  Angeles  basin  and  harbor 
area,  in  A  guide  to  the  geology  and  oil  fields  of  the  Los  Angeles 
and  Ventura  regions:  American  Association  of  Petroleum  Geolo- 
gists ond  Society  of  Economic  Paleontologists  and  Mineralogists, 
Pacific  Sections,  Guidebook,  p.  65-73. 

Rothwell,  W.T.,  Jr.,  1966,  Strotigrophic  focies  prediction  and  recog- 
nition in  young  offshore  basins  from  studies  of  fossil  environ- 
ments: American  Association  of  Petroleum  Geologists  Bulletin,  v. 
50,  p.  650. 

Rowland,  S.M.,  1984,  Geology  of  Sonto  Cotolina  Island  a  review, 
in  Pipkin,  B.W.,  editor.  Geology  of  Sonto  Cotolina  Island  and 
nearby  basins:  Field  Trip  Guidebook  for  Western  Section  of  the 
Notional  Association  of  Geology  Teochers,  p.  1-26. 


102 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


Rubel,  A.C.,  1966,  The  tidelond  development  of  California,  in  OH- 
shore  Exploration  Conference  Proceedings,  Long  Beach,  Califor- 
nio,  p.  1 1-22. 

Rubin,  Dm.,  and  McCulloch,  D.S.,  1976,  Bedform  dynamics  in  San 
Franciso  Bay,  California:  Geological  Society  of  Americo  Ab- 
stracts with  Programs,  v.  8,  p.   1079. 

Rudat,  J.H.,  and  Fischer,  P. J.,  1979,  Quaternary  evolution  and  seis- 
mic strotigraphy  of  the  San  Pedro  Shelf,  southern  California: 
Geological  Society  of  America  Abstracts  with  Programs,  v.  11, 
p.  507. 

Rusnok,  G.A.,  1966,  The  continental  margin  of  northern  and  central 
California:  California  Division  of  Mines  and  Geology  Bulletin 
190,  p.  325-335. 

Soge,  O.G.,  Jr.,  1973,  Paleocene  geography  of  southern  California: 
University  of  Colifornio,  Sonto  Barbaro,  unpublished  Doctorol 
Thesis. 

Samuels,  W.B.,  and  Lanfear,  K.J.,  1980,  An  oil  spill  risk  analysis  for 
the  central  and  northern  Colifornio  (proposed  sale  53)  outer 
continental  shelf  lease  area:  U.S.  Geological  Survey  Open-File 
Report  80-211,  49  p. 

Sanders,  J.E.,  1973,  Map  of  parts  of  floor  of  Sonto  Barbara  Chan- 
nel, California,  compiled  from  side-scanning  sonar  records: 
American  Association  of  Petroleum  Geologists  Bulletin,  v.  57,  p. 
802-803. 

Souto,  A. P.,  1973,  A  bottom  gravity  survey  of  Cormel  Bay,  Colifor- 
nio: U.S.  Naval  Postgroduote  School,  Monterey,  California 
Master's  Thesis,  71  p.;  from  Notional  Technical  Information  Ser- 
vice, U.S.  Deportment  of  Commerce,  Springfield,  Virginia  NTIS- 
A761-377. 

Sovulo,  N.A.,  1978,  Light  mineral  petrology  of  sediments  from  Santo 
Monica  and  Son  Pedro  boys,  Colifornio  continental  borderland: 
University  of  Southern  Colifornio  unpublished  Moster's  Thesis. 

Schneider,  W.A.,  ond  Backus,  M.M.,  1964,  Oceon  bottom  seismic 
measurements  of<  the  Colifornio  coast:  Journal  of  Geophysical 
Reseorch,  v.  69,  p.  1135-1143. 

Scholl,  D.W.,  1959,  Geology  of  surrounding  recent  marine  sediments 
of  Anocopo  Island,  Colifornio:  University  of  Southern  Colifornio 
unpublished  Moster's  Thesis. 

Scholl,  D.W.,  1959,  Exposures  of  San  Onofre  Breccia  on  Anocopo 
Islond,  Colifornio:  American  Association  of  Petroleum  Geologists 
Bulletin,  V.  43,  p.  222  223. 

Scholl,  D.W.,  1960,  Relotionship  of  the  insulor  shelf  sediments  to  the 
sedimentary  environments  and  geology  of  Anocopo  Island,  Cali- 
fornia: Journol  of  Sedimentary  Petrology,  v.  30,  p.   123- 139. 

Schultz,  F.E.,  1971,  Exploration  history  of  the  Sonto  Borboro  Chan- 
nel, in  Explorotion  todoy,  energy  tomorrow:  Society  of  Explora- 
tion Geophysicists,  41st  Annuol  Internotionol  Meeting,  Houston, 
p.  61-62. 

Scloter,  J.G.,  Anderson,  R.N.,  ond  Bell,  ML.,  1971,  Elevation  of 
ridges  and  evolution  of  the  cenlrol  eastern  Pacific:  Journal  of 
Geophysicol  Research,  v.  76,  p.  7888-7915. 

Scott,  E  W.,  ond  Dolton,  G.L.,  1980,  Petroleum  resource  opproisol 
of  proposed  Lease  Sole  73,  offshore  California,  in  McCulloch, 
D.S.,  editor,  A  summary  report  of  the  regionol  geology,  environ- 
mentol  geology.  CCS  resource  opproisol,  petroleum  potential, 
and  operotionol  considerations  in  the  area  of  proposed  Lease 
Sole  73.  offshore  Colifornio:  U.S.  Geological  Survey  Open-File 
Report  80  2007,  p    CI  C6. 

Seeber,  I.,  Borozongi,  M.,  and  Nowrooii,  A.,  1970,  Microeorth- 
quake  seismicity  and  tectonics  of  coostol  northern  California: 
Bulletin  of  the  Seismologicol  Society  of  America,  v.  60,  no.  5,  p. 
1669-1699. 

Seideri,  V.M.,  1979,  Son  Gregorio-Hoigri  foult  zone  south  of  Mon- 
terey Boy,  Colifornio;  A  reduced  estimote  of  moximum  displace- 
ment: U.S.  Geological  Survey  Open  File  Report  79  385,   10  p. 


Semtner,  A.J.,  ond  Grim,  P.J.,  1970,  A  mognetic  ond  bothymetric 
profile  in  the  Pocific  from  the  Cocos  Ridge  to  centrol  California: 
U.S.  Deportment  of  Commerce,  Nationol  Oceonic  and  Atmos- 
pheric Administration,  Atlantic  Oceonogrophic  ond  Meteorologi- 
col  Laboratories,  Collected  Reprints,  v.   I,  10  p. 

Shepard,  F.P.,  1937,  Horizontal  shift  faulting  off  Punto  Gordo,  Cali- 
fornia: Geologicol  Society  of  America  Proceedings,  1936,  p.  101. 

Shepard,  F.P.,  1937,  Sediments  off  the  Colifornio  coast:  American 
Association  of  Petroleum  Geologists  Bulletin,  v.  21,  p.   1614. 

Shepard,  F.P.,  1938,  Colifornio  submorine  canyons:  Geological  Soci- 
ety of  Americo  Bulletin,  v.  49,  p.   1900-1901. 

Shepard,  F.P.,  1938,  Chonging  depths  in  submarine  conyon  heads: 
Geological  Society  of  Americo  Proceedings  1-37,  p.  252. 

Shepard,  F.P.,  1938,  Son  Clemente  submarine  foult:  Geological 
Society  of  America  Proceedings  1937,  p.  252. 

Shepard,  F.P.,  1938,  Structural  trends  off  the  California  coast: 
American  Association  of  Petroleum  Geologists  Bulletin,  v.  22,  p. 
1716. 

Shepard,  F.P.,  1938,  Submarine  canyons  off  ttse  California  coast: 
Colifornio  Journal  of  Mines  ond  Geology,  v.  34,  p.  298-310. 

Shepard,  F.P.,  1939,  Tectonic  development  off  the  Colifornio  coost: 
Oil  Weekly,  v.  93,  p.  69. 

Shepard,  F.P.,  1941,  Non-depositlonal  physiographic  environments 
off  the  California  coast:  Geological  Society  of  America  Bulletin, 
V.  52,  p.  1869-1886. 

Shepard,  F.P.,  1947,  Diving  operations  in  California  submarine  can- 
yons: Geological  Society  of  Americo  Bulletin,  v.  58.  p.   1227 

Shepard,  F.P.,  1948,  Detailed  studies  of  submorine  canyons  ot  La 
Jollo,  California:  Geological  Society  of  America  Bulletin,  v.  59, 
p.  1351. 

Shepord,  F.P.,  1950,  Beach  cycles  in  southern  Colifornio:  U.S.  Army 
Corps  of  Engineers,  Beoch  Erosion  Boord,  Technical  Memoran- 
dum No.  20,  26  p. 

Shepord,  F.P.,  1957,  Northword  continuation  of  the  Son  Andreas 
fault,  Seismologicol  Society  of  Americo  Bulletin,  v.  47,  p.  263. 

Shepord,  F.P.,  1961,  Submarine  canyons  of  the  Son  Diego-Lo  Jollo 
oreo:  Geologicol  Society  of  America  Special  Paper  68,  p.  54. 

Shepord,  F.P.,  ond  Buffington,  E.C.,  1968,  La  Jollo  submarine  fon- 
volley:  Marine  Geology,  v.  6,  p.  107-143. 

Shepord,  F.P.,  Dill,  R.F.,  and  von  Rod,  U.,  1969,  Physiogrophy  ond 
sedimentory  processes  of  Lo  Jollo  submorine  fan-volley,  Colifor- 
nio: American  Association  of  Petroleum  Geologists  Bulletin,  v.  53, 
p.  390-420. 

Shepord,  F.P.,  and  Einsele,  G.,  1962,  Sedimentotion  in  Son  Diego 
Trough  ond  contributing  submarine  canyons:  Sedimentology,  v. 
1,  p.  81-133. 

Shepard,  F.P.,  ond  Emery,  K.O.,  1941,  Submarine  topogrophy  of  the 
Colifornio  coost — conyons  and  tectonic  interpretation:  Geologi- 
cal Society  of  America  Special  Poper,  no.  31,  171  p. 

Shepard,  F  P.,  ond  Emery,  K.O.,   1946,  Submarine  topography  off 

the  Colifornio  coast:  Journol  of  Geology,  v.  54,  p.  306-321. 
Shepard,  F.P.,  GronI,  U.S.,  IV,  ond  Dietz,  R.S.,  1939,  The  emergence 

of  Santo  Cotolino  Island:  American  Journal  of  Science,  v.  237, 

p.  651-655. 
Shepard,  F.P.,  and  Inman,  D.L.,  1951,  Sand  movement  on  the  shol- 

low  inter-conyon  shelf  at  Lo  Jollo,  Colifornio:  US    Beoch  Erosion 

Boord  Technical  Memorandum,  no.  62,  29  p. 
Shepord,   F.P.,  ond  MocDonold.  G.A.,    1938,   Sediments  of  Sonto 

Monica    Boy,    Colifornio:    Americon    Association    of    Petroleum 

Geologists  Bulletin,  v.  22,  p.  201  216. 
Shepard,  F.P.,  and  Marshall,  N.F.,  1969,  Currents  of  Lo  Jollo  and 

Scripps  submarine  canyons:  Science,  v.   165,  p    177- 178 
Shepard.  F  P.,  ond  Morsholl.  N.F..   1973,  Currents  olong  the  floors 

of    submorine    canyons:    American    Association    of    Petroleum 

Geologists  Bulletin,  v.  57.  p.  244  264. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


103 


Shepard,  F.P.,  and  Marshall,  N.F.,  1973,  Storm-generated  current  in 
La  Jollo  submarine  canyon,  California:  Morine  Geology,  v.  15, 
p.  19-24. 

Shepard,  F.P.,  and  Marshall,  N.F.,  1975,  Dives  into  outer  Coronodo 
Conyon  system:  Marine  Geology,  v.  18,  p.  313-323. 

Shepard,  F.P.,  Marshall,  N.F.,  McLoughlin,  P.A.,  1974,  Currents  in 
submarine  canyons:  Deep-Sea  Research,  v.  21,  p.  691-706. 

Shepard,  F.P.,  Revelle,  R.R.,  Dietz,  R.S.,  and  Emery,  K.O.,  1938, 
Coring  off  the  California  coast:  Geological  Society  of  America 
Bulletin,  V.  49,  p.  1900-1901. 

Shepard,  F.P.,  Wood,  F.J.,  and  Sullivan,  G.G.,  1979,  Perigean 
spring  tides  and  unusual  currents  in  La  Jollo  submarine  canyon: 
Geological  Society  of  America  Abstracts  with  Programs,  v.  11, 
p.  515. 

Shepard,  F.P.,  and  Wrath,  W.F.,  Marine  sediments  around  Catolino 
Island:  Journal  of  Sedimentary  Petrology,  v.  7,  p.  41-50. 

Shiller,  A.M.,  and  Price,  N.B.,  1980,  Geochemistry  of  particulate 
matter  in  the  Santa  Barbora  basin,  California:  American  Geo- 
physical Union  Transactions,  v.  61,  p.  269. 

Sholkovitz,  E.,  and  Soutor,  A.,  1975,  Changes  in  the  composition  of 
the  bottom  water  of  the  Santa  Barbara  basin;  effect  of  turbidity 
currents:  Deep-Sea  Research  and  Oceonographic  Abstracts,  v. 
22,  p.  13-21. 

Shor,  G.G.,  Dehlinger,  P.,  Kirk,  H.K.,  and  French,  W.S.,  1968,  Seis- 
mic refraction  studies  off  Oregon  and  northern  California:  Jour- 
nal of  Geophysical  Research,  v.  73,  p.  2175-2194. 

Shor,  G.G.,  and  Raitt,  R.W.,  1958,  Seismic  studies  in  the  southern 
California  borderland:  Congreso  Geologico  Internocionol,  XXa 
Seccion,  1956,  Mexico,  Seccion  IV,  Segundo  Tomo,  p.  243-259. 

Shor,  G.G.,  Raitt,  R.W.,  and  McGowan,  D.D.,  1976,  Seismic  refrac- 
tion studies  in  the  southern  California  borderland,  1949-1974: 
Scripps  Institute  of  Oceanography  Reference  76-13. 

Silberling,  N.J.,  Jones,  D.L.,  Blake,  M.C.,  Jr.,  and  Howell,  D.G., 
1984,  Lithotectonic  terrone  map  of  the  western  conterminous 
United  States,  Part  C,  in  Silberling,  N.J.,  and  Jones,  D.L.,  editors, 
Lithotectonic  terrane  maps  of  the  North  American  Cordillera: 
U.S.  Geological  Survey  Open-File  Report  84-523,  p.  C-1  to  C-33. 

Silver,  E.A.,  1969,  Late  Cenozoic  underfhrusting  of  the  continental 
margin  off  northernmost  California:  Science,  v.  166,  p.  1265- 
1266. 

Silver,  E.A.,  1969,  Structure  of  the  continental  margin  off  northern 
California,  Gordo  escarpment:  American  Geophysical  Union 
Transactions,  v.  50,  p.  207. 

Silver,  E.A.,  1969,  Structure  of  the  continental  margin  off  northern 
California,  north  of  the  Gordo  escarpment:  University  of  Califor- 
nia, Son  Diego,  Scripps  Institution  of  Oceanography,  unpub- 
lished Doctoral  Thesis. 

Silver,  E.A.,  1969,  Tectonic  implications  of  the  structure  of  the  Gordo 
escarpment  and  of  the  magnetic  onomoly  pattern  north  of  the 
escarpment:  Geological  Society  of  America  Abstracts  with  Pro- 
groms,  v.  1,  p.  206-207. 

Silver,  E.A.,  1971,  Tectonics  of  the  Mendocino  triple  junction:  Geo- 
logical Society  of  America  Bulletin,  v.  82,  no.  11,  p.  2965-2978. 

Silver,  E.A.,  1971,  Tronsitional  tectonics  and  late  Cenozoic  structure 
of  the  continental  margin  off  northernmost  California:  Geological 
Society  of  America  Bulletin,  v.  82,  no.  1,  p.  1-22. 

Silver,  E.A.,  1974,  Detailed  near-bottom  geophysical  profile  across 
the  continental  slope  off  northern  California:  U.S.  Geological 
Survey  Journal  of  Reseorch,  v.  2,  p.  563-567. 
Silver,  E.A.,  1974,  Structural  interpretation  from  free-air  gravity  on 
the  Colifornio  continentol  margin,  35  degrees  to  40  degrees 
North:  Geological  Society  of  America  Abstracts  with  Programs, 
V.  6,  p.  253. 
Silver,  E.A.,  1978,  The  Son  Gregorio-Hosgri  fault  zone:  an  overview, 
in  Silver,  E.A.,  and  Normark,  W.R.,  editors,  San  Gregorio-Hosgri 


fault  zone,  California:  California  Division  of  Mines  and  Geology 
Special  Report  137,  p.  1-2. 

Silver,  E.A.,  and  Normark,  W.R.,  editors,  1978,  San  Gregorio-Hosgri 
fault  zone,  California:  California  Division  of  Mines  and  Geology 
Special  Report  137,  54  p. 

Simila,  G.W.,  1980,  Seismologicol  evidence  on  the  tectonics  of  the 
northern  section  of  the  Son  Andreas  fault  region,  in  Streitz,  R., 
and  Sherburne,  R.,  editors.  Studies  of  the  Son  Andreas  fault  in 
northern  Colfornio:  California  Division  of  Mines  and  Geology 
Special  Report  140,  p.  131-138. 

Simila,  G.W.,  Peppin,  W.A.,  and  McEvilly,  T.V.,  1975,  Seismotecton- 
ics  of  the  Cope  Mendocino,  California  area:  Geological  Society 
of  America  Bulletin,  v.  86,  p.  1399-1406. 

Simons,  R.S.,  1977,  Seismicity  of  San  Diego,  1934-1974:  Seismolog- 
icol Society  of  America  Bulletin,  v.  67,  p.  809-826. 

Simons,  R.S.,  1979,  Instrumental  seismicity  of  the  San  Diego  area: 
1934-1978,  in  Abbott,  P.L.,  and  Elliott,  W.J.,  editors.  Earth- 
quakes and  other  perils.  Son  Diego  region:  San  Diego  Associa- 
tion of  Geologists  Publication,  p.  101-105. 

Simpson,  J. P.,  Ill,  1972,  The  geology  of  Cormel  Boy,  California:  U.S. 
Naval  Post  Graduate  School,  Monterey,  California,  unpublished 
Master's  Thesis. 

Smith,  A.G.,  and  Honno,  G.S.,  1952,  A  rare  species  of  chiton  from 
Pioneer  Seamount  off  central  California:  Proceedings  of  the  Cali- 
fornia Academy  of  Sciences,  Fourth  Series,  v.  27,  p.  389-392. 

Smith,  D.L.,  and  Normark,  W.R.,  1976,  Deformation  and  patterns  of 
sedimentation,  south  Son  Clemente  basin,  California  borderland: 
Marine  Geology,  v.  22,  p.  175-188. 

Smith,  M.B.,  1964,  Map  showing  distribution  and  configuration  of 
basement  rocks  in  California:  U.S.  Geological  Survey  Map  OM- 
215. 

Smith,  S.V.,  1970,  Calcium  carbonate  budget  of  the  southern  Cali- 
fornia continental  borderland:  Hawaii  Institute  of  Geophysics 
Report,  HIG-70-11,  174  p. 

Smith,  S.V.,  1971,  Budget  of  calcium  carbonate,  southern  California 
continental  borderland:  Journal  of  Sedimentary  Petrology,  v.  41, 
p.  798-808. 

Smith,  S.W.,  1978,  Sea  floor  expression  of  the  1927  Lompoc  earth- 
quake: American  Geophysical  Union  Tronsoctions,  v.  59,  p. 
1128. 

Smith,  S.W.,  and  Knopp,  J.S.,  1980,  The  northern  termination  of  the 
San  Andreas  fault,  p.  153-164,  in  Streitz,  R.,  and  Sherburne,  R., 
editors.  Studies  of  the  San  Andreas  fault  in  northern  California: 
California  Division  of  Mines  and  Geology  Special  Report  140,  p. 
153-164. 

Smith,  W.S.T.,  1897,  The  geology  of  Santa  Catolino  Island:  Califor- 
nia Academy  of  Science  Proceedings,  3rd  series,  v.  1,  71  p. 

Smith,  W.S.T.,  1898,  The  geological  sketch  of  San  Clemente  Island: 
U.S.  Geological  Survey,  18th  Annual  Report,  p.  465-496. 

Smith,  W.S.T.,  1900,  A  topographic  study  of  the  islands  of  southern 
California:  University  of  California  Publications  in  Geology,  v.  2, 
p.  179-230. 

Smith,  W.S.T.,  1933,  Marine  terraces  on  Santa  Catolina  Island: 
American  Journal  of  Science,  v.  25,  p.   123-136. 

Sonnemon,  H.,  Weaver,  D.W.,  Doerner,  D.P.,  ond  Avilo,  F.A.,  1969, 
Geology  of  Santo  Rosa  Island,  in  Weaver,  D.W.,  editor.  Geology 
of  the  northern  Channel  Islands:  American  Association  of  Petro- 
leum Geologists  and  Society  of  Economic  Paleontologists  and 
Mineralogists,  Pacific  Sections,  Special  Publication. 

Sorenson,  P.E.,  and  Meod,  W.J.,  1969,  A  new  economic  appraisal 
of  marine  phosphorite  deposits  off  the  California  coast,  in  The 
Decade  Ahead,  1970  1980:  Marine  Technology  Society,  5th  An- 
nual Conference,  p.  491-500. 

Sorensen,  S.S.,  1984,  Metamorphic  geology  of  the  Catolino  Schist 
Terrane. on  Santo  Catolino  Island,  in  Pripkin,  B.W.,  editor.  Geol- 
ogy  of   Santo   Catolino   Island   ond   nearby   basins:   Field  Trip 


104 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


Guidebook.  Far  Western  Section  of  the  Nationol  Association  of 
Geology  Teochers,  p.  28-53. 

Sorensen,  S.S.,  1985,  Petroloflic  evidence  for  Jurossic,  island  ore-like 
bosement  rocks  from  the  southwestern  Transverse  Ronges  and 
Colifornio  continental  borderland:  Geological  Society  of  Ameri- 
ca Bulletin,  V.  96,  no.  8,  p.  997-1006. 

Soutor,  A.,  1969,  Sedimentation  in  Santo  Barbara  basin,  California: 
American  Association  of  Petroleum  Geologists  Bulletin,  v.  53,  p. 
468. 

Soutor,  A.,  and  Crill,  PA.,  1977,  Sedimentotion  and  climatic  pat- 
terns in  the  Santa  Barbara  Basin  during  the  19th  and  20th  centu- 
ries: Geological  Society  of  America  Bulletin,  v.  88,  p.  1 1 6 1  - 1 1 72. 

Spikes,  C.H.,  1973,  A  gravimetric  survey  of  the  Santo  Cruz-Afio 
Nuevo  Point  continentol  shelf  and  odjocent  coastline:  U.S.  Novol 
Post-graduate  School,  Monterey,  Colifornio,  Master's  Thesis,  1 14 
p.:  from  Nationol  Technical  Information  Service,  U.S.  Depart- 
ment of  Commerce,  Springfield,  Virginia,  NTIS-A769-431. 

Sprogue,  D.W.,  1971,  Geology  ond  economic  significance  of  Pleis- 
tocene channel  and  terrace  deposits  of  the  Son  Diego  mainland 
shelf,  California:  University  of  Southern  California,  unpublished 
Master's  Thesis. 

Stanley,  E.R.,  and  Stolz,  fH.P.,  Oil  and  gas  explorotion  and  develop- 
ment of  off-shore  oreos:  City  of  Long  Beach  unpublished  report 
0012,  p.  1-17. 

Starke,  G.W.,  and  Howard,  A.D.,  1968,  Polygenetic  origin  of  Mon- 
terey submarine  canyon:  Geological  Society  of  America  Bulletin, 
V.  79,  p.  813-826. 

Stearns,  R.E.C.,  1875,  Discovery  of  fossil  teetfi  of  on  elephant  on 
Santo  Rosa  Island,  Colifornio:  California  Academy  of  Science 
Proceedings,  v.  5,  p.   152. 

Steritz,  J.W.,  1986,  Southern  termination  of  the  Hosgri  fault  zone, 
offshore  California:  Geology  Department,  University  of  Colifor- 
nio at  Santo  Barbara. 

Stevenson,  R.E.,  Conrey,  B.L.,  ond  Gorsline,  D.S.,  1954,  The  inshore 
survey  of  the  Los  Angeles  horbor  approach  orea,  California: 
University  of  Southern  Colifornia,  Deportment  of  Geologicol 
Sciences,  unpublished  report,  208  p. 

Stevenson,  R.E.,  ond  Emery,  K.O.,  1958,  Marshlands  ot  Newport 
Boy,  Colifornio:  University  of  Southern  California,  Allan  Hancock 
Foundation  Occasional  Paper,  no.  20,  109  p. 

Stevenson,  R.E.,  and  Terry,  R.D.,  1957,  Bottom  moteriols  and  topog- 
raphy of  the  shelf  between  Point  Conception  and  Son  Diego,  in 
Oceanography  and  marine  geology  of  the  southern  California 
shelf:  University  of  Southern  Colifornia  Interim  Report  submitted 
to  State  Woter  Pollution  Control  Board,  p.  24-74. 

Stevenson,  R.E.,  Tibby,  R.B.,  and  Gorsline,  D.S.,  1956,  The  oceonog- 
raphy  of  Sonta  Monico  Boy,  California:  University  of  Southern 
Colifornio,  Department  of  Geologicol  Sciences  Report  to  Hyper- 
ion Engineering,  Inc.,  268  p. 

Stevenson,  RE.,  Uchupi,  E.,  and  Gorsline,  D.S.,  1959,  Some  charoc- 
teristics  of  sediments  on  the  mainland  shelf  of  southern  Colifor 
nio,  in  Oceonogrophic  survey  of  the  continental  shelf  areas  of 
southern  California:  California  Stote  Water  Pollution  Control 
Board  Publication  20,  p.  59-109. 

Stewart,  RE.,  1943,  Rincon  oil  field,  in  Geologic  formations  and 
economic  development  of  the  oil  and  gas  fields  of  Colifornio: 
Colifornia  Division  of  Mines  and  geology  Bulletin,  v.  118,  p. 
305390 

Slierman.  D  J.,  and  Ellsworth,  W.L.,  1976,  Aftershocks  of  the  Febru- 
ory  21,  1973  Point  Mugu,  California  eorthquoke:  Seismological 
Society  of  Americo  Bulletin,  v.  66,  p.   1931   1952. 

Stock,  C,  1935,  Exiled  elephonts  of  the  Channel  Islands,  California: 
Scientific  Monthly,  v    41,  p    205-214 

Stock,  C,  1943,  Foxes  and  elephants  of  the  Chonnel  Islands,  Califor- 
nia: los  Angeles  County  Museum  of  Noturol  History  Quarterly 
Report,  v.  3,  p.  6  9. 


Stock,  Cond  Furlong,  E.L.,  1928,  The  Pleistocene  elephants  of 
Santo  Rosa  Isle:  Science,  v.  68,  p.  140141. 

Strand,  R.G  ,  1962,  Geologic  mop  of  Colifornia,  Olaf  P.  Jenkins 
edition.  Redding  Sheet,  California  Division  of  Mines  and  Geol- 
ogy, scale  1:250,000. 

Stuort,  C.J.,  1975,  The  source  terrain  of  the  Son  Onofre  Breccia, 
southern  California:  Geologicol  Society  of  America  Abstracts 
with  Programs,  v.  7,  p.  379. 

Stuart,  C.J.,  1975,  The  stratigraphy,  sedimentology,  ond  tectonic 
implications  of  the  Son  Onofre  Breccio,  southern  California:  Uni- 
versity of  Colifornio,  Santa  Borboro,  unpublished  Doctoral  T)ie- 
sis. 

Stuart,  C.J.,  1976,  Source  terrone  of  the  San  Onofre  Breccia — 
preliminary  notes,  in  Howell,  D.G.,  editor.  Aspects  of  the  geolog- 
ic history  of  the  Colifornio  continentol  borderland:  Americon 
Association  of  Petroleum  Geologists,  Pocific  Section,  Miscellone- 
ous  Publication  24,  p.  309-325. 

Stuort,  C.J.,  1979,  Middle  Miocene  poleogeography  of  coostol 
southern  Colifornio  and  the  Colifornio  borderland;  evidence  from 
schist-bearing  sedimentary  rocks,  in  Armentrout,  J.M.,  Cole, 
M.R.,  and  Terbest,  H.,  Jr.,  editors,  Pocific  Coost  poleogeography 
symposium  3:  Society  of  Economic  Paleontologists  and  Mineralo- 
gists, p.  29-44. 

Sulidikondrotyev,  YD.,  1980,  Foulf  systems  of  the  Pocific:  Geotec- 
tonics,  V.  14,  p.  83-89. 

Summers,  H.J.,  ond  Emery,  K.O,  1963,  Intemol  woves  of  tidol  period 
off  southern  California:  Journal  of  Geophysical  Research,  v.  68, 
p.  827-839. 

Swift,  D.J.L.,  1974,  Continental  shelf  sedimentation,  in  Burk,  C.A., 
and  Drake,  C.L.,  editors.  The  geology  of  continental  margins: 
Springer-Verlog,  p.   117-135. 

Sylvester,  A.G.,  Smith,  S.W.,  and  Scholz,  C.H.,  1968,  Eorthquoke 
swarm  in  the  Santo  Borboro  Channel,  California:  Seismological 
Society  of  America  Bulletin,  v.  60,  p.   1047. 

Szosz,  S.E.,  Fantozzi,  J.H.,  and  Adent,  W.A.,  1969,  Development  of 
Long  Beach  unit  in  offshore  port  of  Wilmington  Field:  American 
Association  of  Petroleum  Geologists  Bulletin,  v.  53,  p.  458. 

Szobo,  B.J.,  ond  Vedder,  J.G.,  1971,  Uronium-series  dating  of  some 
Pleistocene  marine  deposits  in  southern  Colifornia:  Earth  and 
Pionetory  Science  Letters,  v.   11,  p.  283-290. 

Taylor,  J.C,  1976,  California's  developed  ond  undeveloped  border- 
land: American  Association  of  Petroleum  Geologists  Bulletin,  v. 
60,  p.  727. 

Taylor,  J.C,  1976,  Geologicol  approisol  of  the  petroleum  potential 
of  offshore  southern  Colifornio — the  borderland  compared  to 
onshore  coastal  basins:  U.S.  Geological  Survey  Circular  730,  41 

P 

Taylor,  J.C.,  Vedder,  J.G.,  ond  McLean,  H  ,  1975,  Basement  and 
Cenozoic  volcanic  rocks  from  offshore  southern  Colifornio: 
American  Association  of  Petroleum  Geologists,  Annool  Meeting, 
Long  Beach,  California,  p.  8. 

Teng,  T.,  Buiko,  J. A..  Henyey,  T.I.,  McRoney,  J.K.,  Piper,  K.E..  ond 
Sirelitz,  R.A.,  1981,  Earthquake  hozord  research  in  the  los  Ange- 
les basin  and  its  offshore  oreo:  US  Geologicol  Survey  Open-File 
Report  81  295 

Terry,  R.D  ,  1955,  Bibliography  of  marine  geology  and  oceonogro- 
phy,  California  coast:  Colifornio  Division  of  Mines  ar>d  Geology 
Special  Report  44,   131  p. 

Terry,  R.D.,  Kessling,  S.A.,  and  Uchupi,  E.,  1956,  Submarine  geology 
of  Santo  Monica  Boy,  California:  University  of  Southern  Califor- 
nia, Department  of  Geologicol  Sciences  Report  to  Hyperion  Engi- 
neering, Inc.,   177  p. 

Terry,  R  D.,  and  Stevenson,  R.E.,  1957,  Microrelief  of  the  Sonto 
Monico  shelf,  Colifornio:  Geological  Society  of  America  Bulletin, 
V.  68,  p.  125  128. 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


105 


Thatcher,  W.,  and  Hanks,  T.C.,  1973,  Source  parameters  of  southern 
California  earthquakes:  Journal  of  Geophysical  Research,  v.  78, 
p.  8547-8576. 

Theberge,  A.E.,  Jr.,  1971,  Magnetic  survey  off  southern  California 
and  Baja  California:  Notional  Oceanic  and  Atmospheric  Ad- 
mininstration.  National  Ocean  Survey,  Operational  Data  Report, 
NOS  DR-12,  10  p. 

Thenhaus,  P.C,  Perkins,  D.M.,  Ziony,  J. I.,  and  Aigermissen,  S.T., 
1980,  Probabilistic  estimates  of  maximum  seismic  horizontal 
ground  motion  on  rock  in  coastal  California  and  the  adjacent 
outer  continental  shelf:  U.S.  Geological  Survey  Open-File  Report 
80-924. 

Thompson,  G.A.,  and  Tolwoni,  M.,  1964,  Crustal  structure  from  the 
Pacific  basin  to  central  Nevada:  Journal  of  Geophysical  Re- 
search, v.  69,  p.  4813-4837. 

Thompson,  W.C.,  1949,  Ocean  floor  investigations  along  Sonto 
Barbara  County  coast:  American  Association  of  Petroleum 
Geologists  Bulletin,  v.  33,  p.  2062. 

Thompson,  W.C,  1957,  Continental  shelf  structure  and  sediments 
west  of  Santa  Barbara,  California:  Congreso  Internocional  del 
I.N.Q.U.A.  (International  Union  for  Quaternary  Research),  Ac- 
tus, v.  1,  p.  641-646. 

Thornton,  S.E.,  1978,  Suspended  sediment  transport  in  surface  wa- 
ters of  the  southern  California  continental  borderland  after  the 
1977-1978  floods:  Geological  Society  of  America  Abstracts  with 
Programs,  v.  10,  p.  505. 

Thornton,  S.E.,  1980,  Slope-centered  processes  in  Santa  Barbara 
basin,  California  borderland:  American  Association  of  Petroleum 
Geologists  Bulletin,  v.  64,  p.  792-793. 

Thornton,  S.E.,  1981,  Holocene  stratigraphy  and  sedimentary  proc- 
esses in  Santa  Barbara  basin — influence  of  tectonics,  ocean  cir- 
culation, climate,  and  mass  movement:  University  of  southern 
California,  unpublished  Doctoral  Thesis. 

Thornton,  S.E.,  1981,  Suspended  sediment  transport  in  surface  wa- 
ters of  the  California  current  off  southern  California:  1977-78 
floods:  Geo-Marine  Letters,  v.  1,  p.  23-28. 

Thornton,  S.E.,  and  Crissman,  S.,  1979,  Spatial  distribution  of  mass 
movement  in  Santa  Barbara  basin;  sedimentologic  evidence: 
Geological  Society  of  America  Abstracts  with  Programs,  v.  11, 
p.  527-528. 

TIcken,  E.J.,  1983,  Geology  of  the  inner  basin  margin,  Dana  Point 
to  San  Onofre,  California:  California  State  University 
Northridge,  unpublished  Master's  Thesis,  85  p. 

Tooma,  S.G.,  and  Iredale,  H.,  Ill,  1968,  Oceanography  in  the  Chan- 
net  Islands  area  off  southern  California,  September  and  October, 
1965:  U.S.  Naval  Oceanographic  Office  Technical  Report  TR- 
203. 

Toppozada,  T.R.,  Parke,  D.L.,  and  Higgins,  C.T.,  1978,  Seismicity  of 
California  1900-1931:  California  Division  of  Mines  and  Geology 
Special  Report  135. 

Toppozada,  T.R.,  Real,  C.R.,  Bezore,  S.P.,  and  Parke,  D.L.,  1979, 
Compilation  of  pre-1900  California  earthquake  history:  Califor- 
nia Division  of  Mines  and  Geology  Open-File  Report  OFR  79-6, 
SAC,  271  p. 

Townley,  S.D.,  and  Allen,  M.W,,  1939,  Descriptive  catalog  of  earth- 
quakes of  the  Pacific  coast  of  the  United  States,  1769-1928: 
Seismologicol  Society  of  America  Bulletin,  v.  29,  p.  1-297. 

Trask,  B.  1904,  Fossil  Peak,  Santo  Cotalino  Island:  Southern  Califor- 
nia Academy  of  Science  Bulletin,  v.  3,  p.  140. 

Trask,  P.D.,  1928,  Sedimentation  in  the  Channel  Islands  region, 
California:  Economics  of  Geology,  v.  26,  p.  24-43. 

Trask,  P.D.,  1952,  Source  of  beach  sand  at  Santo  Barbara,  Califor- 
nia, as  indicated  by  mineral  groin  studies:  U.S.  Army,  Corps  of 
Engineering,  Beach  Erosion  Board,  Technical  Memorandum  28, 
24  p.;  University  of  California,  Berkeley,  Institute  of  Engineering 
Research,  Series  14,  17  p. 


Truex,  J.N.,  1974,  Structural  evolution  of  Wilmington,  California, 
anticline:  American  Association  of  Petroleum  Geologist  Bulletin, 
V.  58,  p.  2398-2410. 

Truex,  J.N.,  1978,  Pliocene-Pleistocene  diastrophism  of  Santo  Mon- 
ica and  San  Pedro  shelves,  California  continental  borderland, 
discussion:  American  Association  of  Petroleum  Geologist  Bulletin, 
V.  62,  p.  2492-2495. 

Truex,  J.N.,  and  Hunter,  W.H.,  1969,  Development  of  the  offshore 
Wilmington  oil  field:  Society  of  Petroleum  Engineers,  AIME  Pre- 
print, SPE  2562,  p.  1-12. 

Truex,  J.N.,  and  Hunter,  W.H.,  1973,  Development  of  the  offshore 
East  Wilmington  oil  field,  in  Metropolitan  oil  fields  and  their 
environmental  impact:  American  Association  of  Petroleum 
Geologists  and  Society  of  Economic  Paleontologists  and 
Mineralogists  Guidebook,  p.  3-9. 

Tucker,  W.B.,  1927,  Mineral  resources  of  Sonto  Catolino  Island: 
California  State  Mineralogist  Report,  v.  23,  p.  32-39. 

Uchupi,  E.,  1961,  Submarine  geology  of  the  Santa  Rosa-Cortes 
Ridge:  Journal  of  Sedimentary  Petrology,  v.  31,  p.  534-545. 

Uchupi,  E.,  and  Emery,  K.O.,  1963,  The  continental  slope  between 
San  Francisco,  California,  and  Cedros  Island,  Mexico:  Deep-Sea 
Research,  v.  10,  p.  397-447. 

Uchupi,  E.,  and  Gaol,  R.A.P.,  1963,  Sediments  of  the  Polos  Verdes 
shelf,  in  Clements,  T.,  editor.  Essays  in  marine  geology  in  honor 
of  K.P.  Emery:  Southern  California  University  Press,  p.  171-189. 

Uchupi,  E.,  and  Jones,  G.F.,  1967,  Woody  debris  on  the  mainland 
shelf  off  Ventura,  southern  California:  Sedimentology,  v.  8,  p. 
147-151. 

U.S.  Institute  of  Oceanography  (ESSA),  1965,  West  coast  upper 
mantle  project-research  vessel  Pioneer  (1965) :  U.S.  Department 
of  Defence  Gravity  Library. 

U.S.  Institute  of  Oceanography  (ESSA),  1966,  West  coast  upper 
mantle  project-research  vessel  Surveyor  (1966):  U.S.  Depart- 
ment of  Defence  Gravity  Library. 

Upson,  J.E.,  1949,  Late  Pleistocene  and  recent  changes  of  sea  level 
along  the  coast  of  Santa  Barbara  County,  California:  American 
Journal  of  Science,  v.  247,  p.  94-115. 

Upson,  J.E.,  1949,  Former  morine  shorelines  of  the  Govioto  quodron- 
gle,  Santa  Barbara  County,  California:  Journal  of  Geology,  v. 
59,  p.  415-446. 

Valentine,  J.W.,  and  Lipps,  J.H.,  1963,  Late  Cenozoic  rocky  shore 
assemblages  from  Anacopo  Island,  California:  Journal  of  Paleon- 
tology, V.  37,  p.  1292-1302. 

Valentine,  J.W.,  and  Lipps,  J.H.,  1965,  Pleistocene  mollusks  from 
Sonto  Barbara  Island  and  their  biostratigraphic  implications: 
Geological  Society  of  America,  Cordilleran  Section,  61st  Annual 
Meeting,  abstract,  Fresno,  California,  p.  55. 

Valentine,  J.W.,  and  Lipps,  J.H.,  1967,  Late  Cenozoic  history  of  the 
southern  California  islands,  in  Symposium  on  the  biology  of  the 
California  Islonds,  Proceedings;  Santa  Barbara,  California, 
Sonto  Barbara  Botanic  Garden,  p.  21-35. 

Valentine,  J.W,,  and  Veech,  H.H.,  1969,  Rodiometric  ages  of  Pleisto- 
cene terraces  from  Son  Nicolas  Island,  Colifornio:  Geological 
Society  of  America  Bulletin,  v.  80,  p.  1415-1418. 

Van  Dorn,  W.G.,  1979,  Theoretical  aspects  of  tsunamis  along  the 
Son  Diego  coastline,  in  Atbott,  P.L.,  and  Elliott,  W.J.,  editors. 
Earthquakes  and  other  perils.  Son  Diego  Region:  Son  Diego 
Association  of  Geologists  Publication,  p.   115-116. 

Vedder,  J.G.,  1975,  Acoustic  reflection  profiles,  R/V  KELEZ,  May- 
June  1973,  leg  3,  offshore  southern  California:  U.S.  Geological 
Survey  Open-File  Report  75-265,  scale  1:250,000. 

Vedder,  J.G.,  1976,  Precursors  and  evolution  of  the  name  California 
Continental  Borderland,  in  Howell,  D.G.,  editor.  Aspects  of  the 
geologic  history  of  the  California  continental  borderland:  Ameri 
con  Association  of  Petroleum  Geologists,  Pacific  Section,  Miscal- 
loneous  Publication  24,  p.  6-11. 


106 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


Vedder,  J.G.,  Arnol,  RE.,  Barron,  J. A.,  Bokry,  D.,  Crouch,  J.K.,  end 
LeeWong,  F.,  1981,  Composition  and  correlation  of  bedrock  and 
jediment  corej,  R.  V  SEA  SOUNDER  cruije  53  79-SC,  May  1979, 
Colifornio  Continental  Borderland:  U.S.  Geological  Survey 
Open-File  Report  81-744,  74  p. 

Vedder,  J.G.,  Arnol,  J. A.,  Bukry.  D.,  and  Borron,  J. A.,  1976,  Prelimi- 
nary descriptions  of  pre-Quoternory  samples,  R/V  LEE,  March 
1976,  offshore  southern  California:  U.S.  Geological  Survey 
Open-File  Report  76-629,  15  p. 

Vedder,  J.G.,  Arnol,  J. A.,  Bukry,  D.,  ond  Borron,  J.A.,  ond  Lee- 
Wong,  F.,  1979,  Descriptions  of  dart  core  samples,  R  V  SAMUEL 
P.  LEE  cruise  L2-78-SC,  May  1978,  California  continental  border- 
land: U.S.  Geological  Survey  Open-File  Report  76-936,  47  p. 

Vedder,  J.G.,  Beyer,  L.A.  Durhom,  D.L,  Junger,  A.,  McCulloch,  T.H,, 
Roberts,  A.E.,  Taylor,  J.C,  ond  Wagner,  H.C.,  1974,  Geological 
inferences  and  mineral  resource  potentiol  of  the  California  conti- 
nentol  borderlond  north  of  Mexico-US.  boundary:  Speciol  Ad- 
ministration Report  to  Director,  Bureau  of  Land  Monogement, 
Jonuory,   1974,  68  p. 

Vedder,  J.G.,  Beyer,  Junger,  A.,  Moore,  G.W,,  Roberts,  A.E.,  Taylor, 
J.C,  and  Wogner,  H.C.,  1974,  Preliminary  report  on  the  geology 
of  the  continental  borderland  of  southern  California:  U.S.  Geo- 
logical Survey  Miscellaneous  Field  Studies  Mop  MF-624,  34  p. 

Vedder,  J.G.,  Crouch,  J.K,  Arnol,  R.E.,  Bukry,  D.,  Borron,  J. A.,  ond 
Lee-Wong,  F.,  1977,  Description  of  pre-Quoternory  samples,  R''V 
Ellen  B.  Scripps,  September  1976,  Potton  Ridge  to  Bloke  Knolls, 
southern  California  continental  borderlond:  U.S.  Geological  So- 
ciety Open-File  Report  77-474,  19  p. 

Vedder,  J.G.,  Crouch,  J.K,  and  Greene,  H.G.,  1980,  Regional  geol- 
ogy, petroleum  potential,  ond  environmentol  geology  in  the 
southern  port  of  proposed  Lease  Sole  73,  offshore  southern  Coli- 
fornio, in  McCulloch,  D.S.,  editor,  A  summary  report  of  the  re- 
gional geology,  OCS  resource  opproisol,  petroleum  potentiol, 
ond  operotional  considerations  in  the  area  of  proposed  Leose 
Sale  73,  offshore  Colifornio:  U.S.  Geological  Survey  Open-File 
Report  80-2007,  p.  A1-A41. 

Vedder,  J.G.,  Crouch,  J.K,  and  Lee-Wong,  F.,  1981,  Comparotive 
study  of  rocks  from  deep-sea  drilling  project  holes  467,  468,  and 
469  and  the  southern  California  borderland,  in  Posciotto,  K., 
editor.  Leg  63,  Initial  reports,  deep-sea  drilling  project:  U.S. 
Government  Printing  Office,  Washington,  D.C.,  p.  907-918. 

Vedder,  J.G.,  Crouch,  J.K.,  Scott,  E.W.,  Greene,  H.G.,  Cronmer,  D., 
Ibrahim,  M.,  Tudor,  D.,  ond  Vinning,  G.,  1980,  A  summary  report 
of  the  regionol  geology,  petroleum  potentiol,  environmentol  ge- 
ology, and  operation  considerotions  in  the  area  of  proposed 
Leose  Sole  No.  68,  offshore  southern  Colifornio:  U.S.  Geological 
Survey  Open  File  Report  80  198,  62  p. 

Vedder,  J.G.,  Greene,  H.G.,  Scott,  E.W.,  ond  Taylor,  J.C,  1976,  A 
summory  report  of  the  regionol  geology,  petroleum  potential, 
environmentol  geology,  and  technology  for  exploration  and 
development  in  the  oreo  of  proposed  Leose  Sole  No.  48,  Colifor- 
nio continental  borderlond:  U.S.  Geologicol  Survey  Open-File 
Report  76  787,  43  p. 

Vedder,  J.G.,  ond  Hovirell,  D.G.,  1976,  Review  of  the  distribution 
ond  tectonic  implications  of  Miocene  debris  from  the  Cotolino 
Schist,  Colifornio  continentol  borderlond  and  odjocent  coostol 
oreos,  in  Howell,  D.G..  editor.  Aspects  of  the  geologic  history  of 
the  Colifornio  continentol  borderland:  Americon  Association  of 
Petroleum  Geologists,  Pocific  Section,  Miscellaneous  Publicotion 
24,  p.  326  340, 

Vedder,  J.G.,  and  Howell,  D.G.,  1976,  Neogene  stroto  of  the  south- 
ern group  of  Channel  Islonds,  Colifornio,  in  Howell,  D.G.,  editor. 
Aspects  of  the  geologic  history  of  the  California  continental 
borderland:  American  Association  of  Petroleum  Geologists,  Po- 
cific Section,  Miscelloneous  Publication  24,  p.  80  106 


Vedder,  J.G.,  ond  Howell,  D.G.,  1977,  Interrelations  of  Cotolino 
Schist,  Miocene  igneous  rocks,  ond  post-Cretoceous  stroto, 
Sonto  Cotolino  Island,  California:  Geological  Society  of  America 
Abstracts  with  Progroms,  v.  9,  p.   1210. 

Vedder,  J.G.,  and  Howell,  D.G.,  1979,  Geologic  fromewoHt  of  the 
southern  California  borderland:  U.S.  Geological  Survey  Profes- 
sional Paper  1150,  p.   145-147. 

Vedder,  J.G.,  and  Howell,  D.G.,  1979,  Topogrophic  evolution  of  the 
southern  Colifornio  borderland  during  late  Cenozoic  time,  in 
Power,  D.M.,  editor.  The  Colifornio  Islands:  Proceedings  of  o 
Multidisclpllnory  Symposium,  Sonto  Borboro  Museum  of  Natural 
History,  Sonto  Borboro,  Colifornio,  p.  7-31. 

Vedder,  J.G.,  Howell,  D.G.,  and  Formon,  J. A.,  1979,  Miocene  strata 
and  their  relotion  to  other  rocks,  Sonto  Cotolino  Island.  Califor- 
nia, in  Armentrout,  J.M.,  Cole,  MR.,  and  Terbest,  H.,  Jr.,  editors, 
Pocific  coost  poleogeogrophy  symposium  3;  Stotes:  Society  of 
Economic  Paleontologists  ond  Mineralogists,  Pacific  Section,  Los 
Angeles,  p.  239-257. 

Vedder,  J.G.,  ond  Moore,  E.J.,  1976,  Poleoenvironmentol  implico- 
tions  of  fossiliferous  Miocene  and  Pliocene  stroto  on  Son  Cle- 
mente  Island,  Colifornio,  in  Howell,  D.G.,  editor.  Aspects  of  the 
geologic  history  of  the  California  continentol  borderlond:  Ameri- 
can Associotion  of  Petroleum  Geologists,  Pacific  Section,  Miscel- 
loneous Publication  24,  p.  107-135. 

Vedder,  J.G.,  ond  Norris,  R.M.,  1963,  Geology  of  Son  Nicolos 
Islond,  California:  U.S.  Geologicol  Survey  Professional  Paper 
369,  65  p. 

Vedder,  J.G.,  Schoellhomer,  J.E.,  ond  Isroelsky,  M.C,  1956,  Prelimi- 
nory  report  on  the  geology  of  Son  Nicolas  Island,  Colifornio: 
Unnumbered    U.S.    Geological    Survey    Open-File    Report,   Moy 

1956,  prepored  in  cooperotion  with  the  Office  of  Novol  Petro- 
leum Reserves,  Department  of  the  Novy. 

Vedder,  J.G.,  1956,  Preliminary  geologic  mop  of  Son  Nicolas  Island, 
California:  U.S.  Geological  Survey  Open-File  Report,  mop  scale 

1:12,000. 

Vedder,  J.G.,  Schoellhomer,  J.E.,  Norris,  R.M..  ond  Isroelsky,  M.C, 

1957,  Interim  report  on  the  geology  and  oil  possibilities  of  Son 
Nicolas  Island,  California:  U.S.  Geologicol  Survey  Administrative 
report  (Jonuory  1957)  to  Office  of  Novol  Petroleum  Reserves, 
Department  of  the  Novy. 

Vedder,  J.G.,  Scott,  E.W.,  Powers,  R.B.,  Griggs,  D.,  and  Stouffer, 
K.,  1981,  Geologic  fromework,  petroleum  potentiol,  petroleum 
estimotes,  environmental  hazards  and  deep-woter  drilling  tech- 
nology of  the  moritime  boundary  region,  offshore  southern  Coli- 
fornio. in  Powers,  R.B.,  editor,  U.S.  Geological  Survey  Open-File 
Report,  99  p. 

Vedder,  J.G.,  Toylor,  J.C,  Arnol,  RE.,  ond  Bukry,  J.D.,  1976,  Mops 
showing  locotions  of  selected  pre-Quoternory  rock  somples  from 
the  California  continental  borderlond:  U.S.  Geological  Survey 
Miscellaneous  Field  Studies  Mops  MF  737,  3  mops. 

Vedder,  J.G.,  Toylor,  J.C,  Wagner,  H.C,  and  Junger,  A.,  1975, 
Seofloor  bedrock  patterns  from  Potton  Escorpment  to  the  moin- 
lond  shelf  of  southern  Colifornio:  Americon  Association  of  Petro- 
leum Geologists,  Pacific  Section,  Long  Beach,  California. 

Vedder,  J.G.,  ond  Toth,  M.I.,  1976,  Proposed  new  geogrophic 
names  for  features  In  the  California  continental  borderland,  in 
Howell,  D.G.,  editor.  Aspects  of  the  geologic  history  of  the 
Colifornio  continental  borderlond:  Americon  Association  of  Pe- 
troleum Geologists,  Pocific  Section,  Miscellaneous  Publication 
24,  p.  6-11. 

Vedder,  J.G.,  Wogner,  H.C.  and  Schoellhomer,  J.E  ,  1969,  Geologic 
framework  of  the  Sonto  Borboro  Channel  Region,  in  Geology, 
petroleum  developmmt,  ond  selsmlcity  of  the  Sonto  Borboro 
Channel  region,  Colifornio:  U.S.  Geologicol  Survey  Professional 
Paper  679  A,  p    111 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


107 


Ventura,  C.  and  Wintz,  J.,  1971,  Natural  oil  seeps — historical  back- 
ground, in  Straughon,  D.,  editor.  Biological  and  oceanographical 
survey  of  the  Santa  Barbara  Channel  oil  spill  1969-1970 — biolo- 
gy and  bacteriology:  University  of  Southern  California,  Allan 
Hancock  Foundation,  v.  1,  p.  9-16. 

Vernon,  J.W.,  1965,  Final  report  on  shelf  sediment  transport  system: 
University  of  Southern  California,  Department  of  Geological 
Sciences  Report  USC-GEOL.  65-2,  135  p. 

Vernon,  J.V^.,  and  Slater,  R.A.,  1963,  Submarine  tar  mounds,  Santo 
Barbara  County,  California:  American  Association  of  Petroleum 
Geologists  Bulletin,  v.  47,  p.  1624-1627. 

Vickery,  F.P.,  1927,  The  interpretation  of  the  physiography  of  the  Los 
Angeles  coastal  belt:  American  Association  of  Petroleum  Geolo- 
gists Bulletin,  V.  11,  p.  417-424. 

Vogel,  T.M.,  Kvenvolden,  K.A.,  and  Oremlond,  R.S.,  1980,  Hydrocor- 
bon  gases  in  surface  sediments  of  San  Francisco  Bay,  California: 
American  Association  for  the  Advancement  of  Science,  Pacific 
Division,  Abstracts,  61st  Annual  Meeting,  p.  33. 

von  Herzen,  R.P.,  1964,  Ocean  floor  heot-flow  measurements  west 
of  the  United  States  and  Baja  California:  Marine  Geology,  v.  1, 
p.  225-239. 

von  Huene,  R.E.,  1968,  Structural  relation  to  the  Murray  fracture 
zone  and  transverse  ranges:  Proceedings,  Geological  Society  of 
America  Annual  Meeting,  Mexico  City. 

von  Huene,  R.E.,  1969,  Geologic  structure  between  the  Murray  frac- 
ture zone  and  transverse  ranges:  Marine  Geology,  v.  7,  p.  475- 
499. 

von  Huene,  R.E.,  and  Ridlon,  J.B.,  1966,  Offshore  gravity  anomalies 
in  the  Santo  Barbara  Channel,  California:  Journol  Geophysical 
Research,  v.  71,  p.  457-463. 

von  Huene,  R.E.,  and  Scholl,  D.W.,  1969,  Tectonic  implications  of 
structures  in  stratified  sequences  at  the  base  of  Pacific  continen- 
tal margins:  American  Association  of  Petroleum  Geologists  Bulle- 
tin, V.  53,  p.  747-748. 

von  Huene,  R.E.,  1971,  A  possible  relationship  between  the  Trans- 
verse Ranges  of  California  and  the  Murray  Fracture  zone:  Geo- 
logical Society  of  America  Abstracts  with  Programs,  v.  3,  p.  213. 

von  Huene,  R.E.,  Corbato,  C.E.,  and  Harrison,  J.C,  1965,  Preliminary 
interpretation  of  a  gravity  map  of  the  southern  borderland  off 
southern  California:  American  Geophysical  Union  Transactions, 
V.  46. 

von  Huene,  R.E.,  and  Kulm,  LD.,  1973,  Sites  173,  178,  179,  180, 
181,  and  182,  description  and  synthesis:  in  Kulm,  L.D.,  von 
Huene,  R.  and  others.  Initial  reports  of  the  Deep  Sea  Drilling 
Project,  U.S.  Government  Printing  Office,  Washington,  D.C.,  v. 
XVIII. 

von  Huene,  R.E.,  and  Kulm,  L.D.,  1973,  Tectonic  summary  of  Leg  18, 
in  Kulm,  L.D.,  von  Huene,  R.E.,  and  others,  1973,  Initial  reports 
of  the  deep  sea  drilling  project:  U.S.  Government  Printing  Office, 
Washington,  D.C.,  v.  XVIII. 

von  Huene,  R.E.,  and  Ridlon,  J.B.,  1965,  Offshore  gravity  and  mag- 
netic anomalies  in  the  Santa  Barbara  Channel,  California:  Naval 
Ordinance  Test  Station,  Technical  Publication  3917,  52  p. 

von  Huene,  RE.,  and  Ridlon,  J.B.,  1966,  Offshore  gravity  anomalies 
in  the  Santo  Barbara  Channel,  California:  Journal  of  Geophysi- 
cal Research,  v.  71,  p.  457-465. 

von  Rod,  U.,  1968,  Comparison  of  sedimentation  in  the  Bavarian 
flysch  (Cretaceous)  and  recent  Son  Diego  trough:  Journal  of 
Sedimentary  Petrology,  v.  38,  p.  1120-1154. 

Wagner,  H.C.,  1974,  Marine  geology  between  Cape  San  Martin  and 
Point  Sol  south-central  Colifornio  offshore:  U.S.  Geological  Sur- 
vey Open-File  Report  74-252. 

Wagner,  H.C.,  1975,  Seismic  reflection  profiles  R/V  KELEZ,  May 
1973,  Leg  2,  offshore  southern  California:  U.S.  Geological  Sur- 
vey Open-File  Report  74-205. 


Wagner,  H.C.,  1975,  Geologic  mop  of  offshore  area  between  Point 
Estero  and  Point  San  Luis,  south-central  California:  U.S.  Geologi- 
cal Survey  Administrative  Report,  scale  1:84,000. 

Wagner,  H.C.,  1975,  Tectonic  map  of  offshore  area  between  Point 
Sol  and  Point  Arguello,  south-central  California:  U.S.  Geological 
Survey  Administrative  Report,  scale  1:125,000. 

Wagner,  H.C.,  and  Junger,  A.,  1972,  Late  Tertiary  tectonic  develop- 
ment of  Santo  Monica  basin,  California:  Geological  Society  of 
America  Abstracts  with  Programs,  v.  7,  p.  383-384. 

Wagner,  H.C.,  Wolf,  S.C,  McCulloch,  D.S.,  Silver,  E.A.,  Greene, 
J.G.,  and  Blom,  K.G.,  1972,  Unconsolidated  sediment  thickness 
on  continental  shelf  of  California:  U.S.  Geological  Survey  Ad- 
ministrative Report  prepared  and  furnished  to  U.S.  Bureau  of 
Reclamation  for  California  Undersea  Aqueduct  study,  32  maps, 
scale  1:125,000. 

Wagner,  H.C.,  Wolf,  S.C,  McCulloch,  D.S.,  Silver,  E.A.,  Greene, 
J.G.,  Blom,  K.G.,  and  Junger,  A.,  1973,  Preliminary  geologic  map 
of  continental  shelf  of  California:  U.S.  Geological  Survey  Ad- 
ministrative Report  prepared  and  furnished  to  U.S.  Bureau  of 
Reclamation  for  California  Undersea  Aqueduct  study,  scale  1:- 
125,000. 

Wahrhoftig,  C,  and  Rowntree,  R.,  1972,  Bolinas  Lagoon,  a  problem 
in  coastal  environmental  management:  Geological  Society  of 
America,  Abstracts  with  Programs,  v.  4,  p.  254. 

Walker,  R.G.,  1980,  Modern  and  ancient  submarine  fans:  Reply: 
American  Association  of  Petroleum  Geologist  Bulletin,  v.  64,  p. 
1101-1108. 

Warme,  J.E.,  1966,  Poleoecological  aspects  of  the  recent  ecology  of 
Mugu  Lagoon,  California:  University  of  California,  Los  Angeles, 
unpublished  Doctoral  Thesis. 

Waylond,  R.G.,  Acuff,  A.D.,  McCullooh,  T.H.,  Raleigh,  C.B.,  Vedder, 
J.G.,  and  Yenne,  K.A.,  1978,  Facts  relating  to  Well  No.  5,  Pitas 
Point  Unit  area,  and  the  earthquake  of  August  13,  1978,  Santo 
Barbara  Channel,  California:  U.S.  Geological  Survey  Open-File 
Report  78-906,  67  p. 

Weaver,  D.W.,  editor,  1969,  Geology  of  the  northern  Channel  Is- 
lands: American  Association  of  Petroleum  Geologists  and  Soci- 
ety of  Economic  Paleontologists  and  Mineralogists,  Pacific 
Sections,  Special  Publication,  200  p. 

Weaver,  D.W.,  1969,  Poleogeographic  implications  and  geologic 
history,  in  Weaver,  D.W.,  editor.  Geology  of  the  northern  Chan- 
nel Islands:  American  Association  of  Petroleum  Geologists  and 
Society  of  Economic  Paleontologists  and  Mineralogists,  Pacific 
Sections,  Special  Publication,  p.  115-124. 

Weaver,  D.W.,  1969,  General  geology  of  the  region,  in  Weaver, 
D.W.,  editor.  Geology  of  the  northern  Channel  Islands,  southern 
California  borderland:  American  Association  of  Petroleum 
Geologists  and  Society  of  Economic  Paleontologists  and 
Mineralogists,  Pacific  Sections,  Special  Publication,  p.  9-10. 

Weaver,  D.W.,  1969,  The  Cretaceous  rocks,  in  Weaver,  D.W.,  edi- 
tor. Geology  of  the  northern  Channel  Islands:  American  Associa- 
tion of  Petroleum  Geologists  and  Society  of  Economic 
Paleontologists  and  Mineralogists,  Pacific  Sections,  Special  Pub- 
lication, p.  14-16. 

Weaver,  D.W.,  1969,  The  pre-Tertiory  rocks,  in  Weaver,  D.W., 
editor.  Geology  of  the  northern  Channel  Islands:  American  As- 
sociation of  Petroleum  Geologists  and  Society  of  Economic  Pa- 
leontologists and  Mineralogists,  Pacific  Sections,  Special 
Publication,  p.   1 1-13. 

Weaver,  D.W.,  and  Doerner,  DP.,  1967,  Western  Anocopo — a  sum- 
mary of  the  Cenozoic  history  of  the  northern  Channel  Islands:  in 
Philbrick,  R.,  editor.  Proceedings  of  the  symposium  on  the  biology 
of  the  California  Islands:  Santo  Barbara,  California,  Santo  Bar- 
bara Botanic  Garden,  p.  13-20. 

Weaver,  D.W.,  and  Doerner,  D.P.,  1969,  Lower  Tertiary  stratigra- 
phy, San  Miguel  and  Santa  Rosa  Islands,  in  Weaver,   D.W., 


108 


DIVISION  OF  MINES  AND  GEOLOGY 


BULLETIN  207 


editor,  Geology  of  the  northern  Channel  Islands:  American  As- 
sociation of  Petroleum  Geologists  and  Society  of  Economic  Pa- 
leontologists and  Minerologists,  Pacific  Sections,  Special 
Publicotion,  p.  30-47, 

Weaver,  D.W.,  and  Doerner,  D.P.,  1969,  Mid-Tertiary  stratigraphy, 
San  Miguel  Island,  in  Weaver,  D.W.,  editor.  Geology  of  the 
northern  Channel  Islands:  American  Association  of  Petroleum 
Geologists  and  Society  of  Economic  Paleontologists  and 
Mineralogists,  Pocific  Sections,  Special  Publication,  p.  80-84. 

Weaver,  D.W.,  Griggs,  G.,  McClure,  D.V.,  and  McKey,  J.R.,  1969, 
Volcaniclastic  sequence,  south-central  Santo  Cruz  Island,  in 
Weaver,  D.W.,  editor,  Geology  of  the  northern  Channel  Islands: 
American  Association  of  Petroleum  Geologists  and  Society  of 
Economic  Paleontologists  and  Mineralogists,  Pacific  Sections, 
Special  Publication,  p.  85-90. 

Weaver,  D.W.,  and  Meyer,  G.L.,  1969,  Stratigraphy  of  northeastern 
Santa  Cruz  Island,  in  Weaver,  D.W.,  editor.  Geology  of  the 
northern  Channel  Islands:  American  Association  of  Petroleum 
Geologists  and  Society  of  Economic  Paleontologists  and 
Mineralogists,  Pacific  Sections,  Special  Publication,  p.  95-104. 

Weaver,  D.W.,  and  Wilhelm,  V.H.,  1943,  Huntington  Beach  oil  field, 
in  Geologic  formations  ond  economic  development  of  the  oil  and 
gas  fields  of  California:  California  Division  of  Mines  Bulletin  1 18, 
p.  329-331. 

Weber,  F.H.,  Jr.,  1963,  Geology  and  mineral  resources  of  San  Diego 
County,  California:  California  Division  of  Mines  and  Geology 
County  Report  3. 

Weber,  G.E.,  ond  Cotton,  W.R.,  1981,  Geologic  investigation  of 
recurrence  intervals  and  recency  of  faulting  along  the  Son  Gre- 
gorio  foult  zone,  San  Mateo  County,  Colifornio:  U.S.  Geological 
Survey  Open-File  Report  81-263,  p.  133. 

Weber,  G.E.,  ond  LoJoie,  K.R.,  1977,  Late  Pleistocene  and  Holocene 
tectonics  of  the  Son  Gregorio  fault  zone  between  Moss  Beach 
and  Point  Ano  Nuevo,  Son  Mateo  County,  California:  Geological 
Society  of  America  Abstracts  with  Programs,  v.  9,  p.  524. 

Weber,  G.E.,  ond  LoJoie,  K.R.,  1980,  Mop  of  Quaternary  faulting 
olong  the  San  Gregorio  fault  zone.  Son  Mateo  and  Santa  Cruz 
counties,  California:  U.S.  Geological  Survey  Open-File  Report 
80-709,  scale  1:24,000. 

Weeks,  L.A.,  and  Lottimore,  R.K.,  1971,  Continental  terrace  and 
deep  plain  offshore  central  Colifornio:  U.S.  Deportment  of  Com- 
merce, Notional  Oceanic  and  Atmospheric  Administrotion,  At- 
lantic Oceonogrophic  ond  Meteorological  Laborotories, 
Collected  Reprints,  v.  2,  17  p. 

Wehmiller,  J.F.,  1982,  A  review  of  amino  acid  rocemizotion  studies 
in  Quaternary  mollusks:  strotigrapoic  and  chronologic  applica- 
tions in  coastal  and  interglociol  sites.  Pacific  and  Atlantic  coasts. 
United  States,  United  Kingdom,  Baffin  Island,  and  tropical  island: 
Quoternory  Science  Reviews,  v.  1,  p.  83-120. 

Wehmiller,  J.F.,  La  Joie,  K.R.,  Kvenvolden,  K.A.,  Peterson,  E.,  Belk- 
nap, D.F.,  Kennedy,  G.L.,  Addicott,  W.O.,  Vedder,  J.G.,  and 
Wright,  R.W.,  1977,  Correlation  and  chronology  of  Pacific  coast 
murine  terroce  deposits  by  fossil  omino-ocid  stereochemistry 
technique,  evaluation,  relative  ages,  kinetic  model  ages  and 
geologic  implications:  U.S.  Geological  Survey  Open-File  Report 
77  680,  191  p.  18  figures,  13  tables. 

Wehmiller,  J.F.,  Peterson,  E.,  Kvenvolden,  K.A.,  Lojoie,  K.R.,  ond 
Wright,  R.W.,  1974,  Amino  ocid  enantiomeric  rotios  as  correlo 
tive  and  chronologic  tools  in  the  study  of  Colifornio  marine  ter- 
roces:  Americon  Geophysical  Union  Transactions,  v.  55,  p    1 139 

Weldoy,  E.E.,  ond  Williams,  J.W.,  1975,  Offshore  surficiol  geology 
of  California:  California  Division  of  Mines  and  Geology  Map 
Sheet  26. 

Weser,  O.E.,  1977,  Deep-water  oil  sand  reservoirs,  ancient  cose 
histories  and  modern  concepts:  American  Association  of  Petro- 


leum Geologists  Continuing  Education  Course  Notes  Series  6, 
169  p. 

Wesson,  R.L.,  Bennett,  RE.,  and  Meagher,  K.L.,  1972a,  Catolog  of 
eorthquokes  along  the  Son  Andreas  fault  system  in  centrol  Cali- 
fornia, Jonuory  ■  March,  1972:  U.S.  Geological  Survey  Open-File 
Report,  60  p. 

Wesson,  R.I.,  Bennett,  R.E.,  and  Lester,  F.W.,  1972b,  Catolog  of 
eorthquokes  olong  the  San  Andreas  foult  system  in  central  Cali- 
fornia, April  -  June,  1972:  U.S.  Geological  Survey  Open-File 
Report,  42  p. 

Wesson,  R.L.,  Meogher,  K.L.,  and  Lester,  F.W.,  1973b,  Catolog  of 
earthquakes  along  the  San  Andreas  fault  system  in  central  Cali- 
fornia, July  -  September,  1972:  U.S.  Geological  Survey  Open- 
File  Report,  49  p. 

Wesson,  R.L.,  Lester,  F.W.,  ond  Meagher,  1974o,  Catalog  of  eartfi- 
quakes  along  the  San  Andreas  fault  system  in  centrol  California, 
October  ■  December,  1972:  U.S.  Geological  Survey  Open-File 
Report,  46  p. 

Wesson,  R.L.,  Lester,  F.W.,  and  Meagher,  K.L.,  1974b,  Catalog  of 
earthquakes  along  the  San  Andreas  fault  system  in  central  Coli- 
fornio, Jonuory  -  March  1973:  U.S.  Geological  Survey  Open-File 
Report,  46  p. 

West,  J.W.,  1955,  Geology  of  the  southwestern  port  of  the  Malibu 
Beach  quadrangle,  Los  Angeles  County,  California:  University  of 
California,  Los  Angeles,  unpublished  Master's  Thesis. 

Wiegand,  J.W.,  1970,  Evidence  of  a  San  Diego  Bay-Tijuana  foult: 
Association  of  Engineering  Geologists  Bulletin,  v.  7,  p.  107-121. 

Wilcox,  R.E.,  Harding,  T.P.,  and  Seely,  D.R.,  1973,  Basic  wrench 
tectonics:  American  Associotion  of  Petroleum  Geologists,  v.  57, 
p.  74-96. 

Wilde,  P.,  1965,  Estimates  of  bottom  current  velocities  from  groin 
size  measurements  for  sediments  from  the  Monterey  deep-sea 
fan:  Marine  Technological  Society-American  Littoral  Society  Pro- 
ceedings, V.  2,  p.  718-727. 

Wilde,  P.,  1965,  Recent  sediments  of  the  Monterey  deep-sea  fan: 
Harvard  University,  unpublished  Doctoral  Thesis. 

Wilde,  P.,  1965,  Recent  sediments  of  the  Monterey  deep-sea  fan: 
University  of  California,  Berkeley,  Hydrology  Engineering  Lobo- 
rotory  Report  HEL  2-13,   153  p. 

Wilde,  P.,  Normark,  W.R.,  ond  Chose,  T.E.,  1976,  Oceonogrophic 
doto  off  central  California,  37  degrees  to  40  degrees  North 
including  the  Delgodo  deepseo  fon:  University  of  Colifornio, 
Berkeley,  Lawrence  Berkeley  Loborotory  Publication  number  92. 

Wilde,  P.,  Normork,  W.R.,  and  Chose,  T.E.,  1976,  Petroleum  poten- 
tial of  continental  rise  off  central  Colifornio — summary,  in  Cir- 
cum-Pocific  energy  and  mineral  resources:  Americon  Association 
of  Petroleum  Geologists  Memorandum  25,  p.  313-317. 

Wilde,  P.,  Normark,  W  R.,  and  Chose,  T.E.,  1978,  Channel  sands  ond 
petroleum  potentiol  of  Monterey  deep-sea  fan,  California: 
American  Association  of  Petroleum  Geologists  Bulletin,  v.  62,  p. 
967  983. 

Wilde,  P.,  Normark,  W  R.,  and  Chose,  T.E.,  1980,  Potentiol  petro 
leum  reservoirs  on  deepseo  fans  off  central  California:  Americon 
Association  of  Petroleum  Geologists  Bulletin,  v    64,  p.  803. 

Wildhorber,  J.L.,  1966,  Suspended  sediment  over  the  continentol 
shelf  off  southern  Colifornio:  University  of  Southern  California, 
unpublished  Master's  Thesis. 

Wilkinson,  E.R.,  1972.  Colifornio  offshore  oil  ond  gas  seeps:  Califor- 
nia Division  of  Oil  ond  Gas  Report,   1 1  p. 

Willis,  D.K.,  1979,  Texturol  comporiion  of  insular  ond  moinlond  shelf 
sediments,  continental  borderland,  Colifornio:  University  of 
Southern  California,  unpublished  Master's  Thesis. 

Willis,  R.B.,  1958,  Sunset  Beach  oil  field,  in  Higgins,  J.W.,  editor,  A 
guide  to  the  geology  and  oil  fields  of  the  los  Angeles  ond 
Venluro  regions:  American  Association  of  Petroleum  Geologists, 
Pacific  Section,  p    88 


1987 


GEOLOGY  OF  THE  CALIFORNIA  CONTINENTAL  MARGIN 


109 


Wilson,  J.C.,  Jr.,  1970,  Engineering  properties  of  southern  California 
borderland  sediments:  University  of  Soutfiern  California,  unpub- 
lished Master's  Thesis. 

Wilson,  T.A.,  and  Mero,  J.L.,  1966,  Economic  deposits  of  the  Califor- 
nia offshore  area,  in  Streitz,  R.,  and  Sherburne,  R.,  editors.  Geol- 
ogy of  northern  California:  California  Division  of  Mines  and 
geology  Bulletin  190,  p.  343-353. 

Wimberly,  C.S.,  1955,  Marine  sediments  north  of  Scripps  submarine 
canyon.  La  Jolla,  California:  Journal  of  Sedimentary  Petrology, 
V.  25,  p.  24-37. 

Wimberly,  C.S.,  1963,  Sediments  of  the  mainland  shelf  near  Santa 
Barboro,  California,  in  Clements,  R.,  editor.  Essays  in  marine 
geology  in  honor  of  K.O.  Emery:  Southern  California  University 
Press,  p.  191-201. 

Wimberly,  C.S.,  1964,  Sediments  of  the  southern  Calif ornio  main- 
lond  shelf:  University  of  Southern  California,  unpublished  Doc- 
toral Thesis. 

Winterer,  E.L.,  Curroy,  J.R.,  and  Peterson,  M.N. A.,  1968,  Geologic 
history  of  the  intersection  of  Pioneer  Fracture  zone  with  Delgada 
Deep-Sea  fan,  northeast  Pacific:  Deep-Seo  Research,  v.  15,  p. 
509-520. 

Winterer,  E.L.,  Hawkins,  J.W.,  Matthews,  J.L.,  and  Allison,  E.C., 
1969,  Inverted  metomorphic  zonotion  of  Franciscan  rocks  of  the 
California  borderland — possible  relation  to  Mesozoic  continental 
underthrusting:  Geological  Society  of  America  Abstracts  with 
Programs,  v.  1,  p.  240-241. 

Wolf,  S.C.,  1968,  Current  patterns  and  mass  transport  of  clastic 
sediments  over  the  shelf  regions  of  Monterey  Boy:  San  Jose  State 
College,  unpublished  Master's  Thesis. 

Wolf,  S.C,  1970,  Sedimentation  and  coastal  currents  over  the  shelf 
regions  of  Monterey  Boy:  Marine  Geology,  v.  8,  p.  321-336. 

Wolf,  S.C,  1975,  Seismic  reflection  profiles,  R/V  POLARIS,  March 
1972,  offshore  southern  Colifornio,  Point  Conception  cruise:  U.S. 
Geological  Survey  Open-File  Report  75-166,  22  p. 

Wood,  H.O.,  1947,  Earthquakes  in  southern  Colfornia  with  geologic 
relations  (Parts  I  and  II) :  Seismological  Society  of  America  Bulle- 
tin, v.  37,  p.  217-258. 

Wood,  H.O.,  and  Heck,  N.H.,  1951,  Earthquake  history  of  the 
United  States.  Port  II — Stronger  earthquakes  of  California  and 
western  Nevada:  U.S.  Coast  and  Geodetic  Survey,  Serial  609, 
35  p. 

Woodford,  A.O.,  1924,  The  Catalino  metomorphic  facies  of  the 
Franciscan  series:  Department  of  Geological  Sciences  Bulletin, 
California  University,  v.  15,  no.  3,  p.  49-68. 

Woodford,  A.O.,  1925,  The  Son  Onofre  Breccia:  University  of  Cali- 
fornia Publications  in  Geological  Sciences,  v.  15,  p.  159-280. 

Woodford,  A.O.,  1951,  Stream  gradients  and  Monterey  Sea  Valley: 
Geologic  Society  of  America  Bulletin,  v.  62,  p.  799-852. 

Woodford,  A.O.,  and  Bailey,  T.L.,  1928,  Northwestern  continuation 
of  the  San  Onofre  Breccia:  University  of  California  Publications 
in  Geological  Sciences,  v.  17,  p.  187-191. 

Woodford,  A.O.,  and  Gander,  C,  1977,  Los  Angeles  erosion  surface 
of  middle  Cretoceous  age:  American  Association  of  Petroleum 
Geologists  Bulletin,  v.  61,  p.  1979-1990. 

Woodford,  A.O.,  and  Howell,  D.G.,  1980,  Eocene  conglomerate 
sedimentology  and  basin  analysis.  Son  Diego  and  the  southern 
California  borderland  discussion  and  reply:  Journal  of  Sedimen- 
tary Petrology,  v.  50,  p.  655-656. 

Woodford,  A.O.,  Schoellhamer,  J.E.,  Vedder,  .G.,  and  Yerkes,  R.F., 
1954,  Geology  of  the  Los  Angeles  Bosin,  in  Johns,  R.H.,  editor. 
Geology  of  southern  California:  California  Division  of  Mines  and 
Geology  Bulletin  170,  p.  65-81. 

Woodring,  W.P.,  1957,  Marine  Pleistocene  of  California,  in  Lodd, 
H.S.,  editor.  Treatise  on  marine  ecology  and  paleontology:  Geo- 
logical Society  of  America  Memoir  67,  v.  2,  p.  589-598. 


Woodring,  W.P.,  and  Bramlette,  M.N.,  1950,  Geology  and  paleon- 
tology of  the  Santo  Maria  district,  California:  U.S.  Geological 
Survey  Professional  Paper  222,  185  p. 

Woodring,  W.P.,  Bromlette,  M.N.,  Kew,  W.S.W.,  1946,  Geology 
and  paleontology  of  the  Polos  Verdes  Hills,  California:  U.S.  Geo- 
logical Survey  Professional  Paper  207,  145  p. 

Woodson,  W.B.,  III,  1973,  A  bottom  gravity  survey  of  the  continental 
shelf  between  Point  Lobos  and  Point  Sur,  California:  U.S.  Post 
Graduate  School,  Monterey,  California,  unpublished  Master's 
Thesis. 

Woodson,  W.B.,  III,  1973,  An  underwater  gravity  survey  of  the 
seafloor  between  Point  Lobos  and  Point  Sur,  California:  U.S.  Post 
Graduate  School,  Monterey,  California,  Master's  Thesis,  1 10  p., 
from  National  Technical  Information  Service,  U.S.  Department  of 
Commerce,  Springfield,  Virginia,  NTIS-A769-406. 

Wornardt,  W.W.,  Jr.,  1973,  Diatom,  silicoflogellote,  radiolarion, 
colcoreous  nonnofossil,  and  foraminiferal  biostrotigrophy  of  the 
middle  and  late  Miocene  and  Ploicene  of  Newport  Back  Bay, 
Newport  Beach,  California:  Society  of  Economic  Paleontologists 
and  Mineralogists,  Pacific  Sections,  Guidebook,  Trip  1,  p.  39-53. 

Wroth,  W.F.,  1936,  Marine  sedimentation  around  Catalino  and  San 
Clemente  Island:  University  of  Illinois,  unpublished  Master's  The- 
sis. 

Wright,  F.F.,  1967,  Marine  geology  of  San  Miguel  Gap  off  Point 
Conception,  California:  University  of  Southern  California,  unpub- 
lished Doctoral  Thesis. 

Wright,  F.F.,  1967,  The  marine  geology  of  Son  Miguel  Gap  off  Point 
Conception,  California:  Dissertation  Abstracts  International,  v. 
28,  p.  238B-239B. 

Yancey,  R.E.,  and  Lee,  J.W.,  1972,  Major  heavy-mineral  assem- 
blages and  heavy  mineral  provinces  of  central  California  coast 
region:  Geological  Society  of  America  Bulletin,  v.  83,  p.  2099- 
2104. 

Yates,  L.G.,  1889,  Preliminary  notes  on  the  geology  of  the  Anacopas 
West:  The  American  Geologist,  v.  6,  p.  155-156. 

Yotes,  L.G.,  1890,  Notes  on  the  geology  and  scenery  of  the  islands 
forming  the  southerly  line  of  the  Santa  Barbara  Chonnel:  The 
American  Geologist,  v.  5,  p.  43-52. 

Yates,  L.G.,  1890,  Stray  notes  on  the  geology,  mollusca,  and  insular 
floras  of  the  Channel  Islands:  California  Stote  Mineralogist,  9th 
Annual  Report,  p.  161-188. 

Yotes,  L.G.,  1892,  Peculiar  geologic  processes  on  the  Channel  Is- 
lands of  California:  Geological  Society  of  America  Bulletin,  v.  3, 
p.  133. 

Yeats,  R.S.,  1968,  Rifting  and  rafting  in  the  southern  California 
borderland,  in  Dickinson,  W.R.,  and  Grontz,  A.,  Proceedings  of 
conference  on  geologic  problems  of  Son  Andreas  foult  system: 
Stanford  University  Publication  in  Geologicol  Sciences,  v.  1 1,  p. 
307-320. 

Yeats,  R.S.,  1968,  Southern  Colifornio  structure,  sea  floor  spreading, 
and  history  of  the  Pacific  basin:  Geological  Society  of  America 
Bulletin,  V.  79,  p.  1693-1702. 

Yeats,  R.S.,  1969,  Anocapo  rift,  California:  American  Association  of 
Petroleum  Geologists  Bulletin,  v.  53,  p.  460. 

Yeats,  R.S.,  1970,  Strotigraphic  evidence  for  Catalino  Schist  base- 
ment north  of  Channel  Islands,  California:  Geological  Society  of 
America  Bulletin,  v.  81,  p.  2147-2152. 

Yeats,  R.S.,  1971,  East  Pacific  Rise  and  Miocene  tectonics  of  the 
southern  Ventura  basin:  Geological  Society  of  America  Bulletin, 
V.  3,  p.  222. 

Yeats,  R.S.,  1973,  Newport-lnglewood  fault  zone,  Los  Angeles  basin, 
California:  American  Association  of  Petroleum  Geologists  Bulle- 
tin, V.  57,  p.  117-135. 

Yeats,  R.S.,  1976,  Extension  versus  strike-slip  origin  of  the  southern 
California  continental  borderland,  in  Howell,  D.G.,  editor.  As- 
pects of  the  geologic  history  of  the  Colifornio  borderland:  Ameri- 


THIS  BOOK  IS  DUE  ON  THE  LAST  DATE 
STAMPED  BELOW 

BOOKS  REQUESTEO~^^OTHER  BORROWER 
ARE  SUBJECT  TO  IMMEDIATE  RECALL 


SEf^25l997 
^M  -  7  1998 

APR  I  0  1998 
L.      PSL 
r    MAft  2  b  1999 
RECEIVED 
I     APR  2  9  1999 
I  PSL 


hiL/^^;!:"'"""^'^ °' California,  dav.s 


,^ 


UNIVEHSITV  OF  CALIf 


3  1175  02103  8065 


-0.8    w 

Q 

Z 

o 

o 

IJJ 

1.2   w 


1.6 


CALIFORNIA  CONTINENTAL  MARGIN  GEOLOGIC  MAP  SERIES 

MASTER  LEGEND  AND  EXAMPLE  SEISMIC  REFLECTION  PROFILES 

WITH  SYMBOLS  AND  TERMINOLOGY.  (PLATE  1) 


300- 

600- 

ti!    900- 


1800. 


1200-     -_. 


1500- 


0.4 
0.8 


COLLATE : 
^         PIECES 


9U 

m 

H 
II 
ui 

81 

y 
p 


s 


DIVISION  OF  MINES  AND  GEOLOGY 

BRIAN  E,  TUCKER,    ACTING   STATE  GEOLOGIST 


STATE  OF  CALIFORNIA-GEORGE  DEUKMEJIAr 

THE  RESOURCES  AGENCY -GORDON  K  VAN  VLECK,  SECHEl 
DEPARTMENT  OF  CONSEHVATION-RANDALL  M  WA 


Master  Legend  orSiratigraphic  Units 

I     Q     I  LifKoriolidaKiJ  deposits  of  Quaiernaiy  age 
Of       FandcposibofQuaieTnary  age 
Od       DcM;iicdep<Hitso(  Quaternary  age 
Igjjm'l  Deliait  depcKiu  of  QuBicrnnry  age  overlain  by  ihick  (grcaKr  ihon  3m  i  dcpasiis  of  Q 
[  Qcf   I  (  .iFni>n  or  channel  fill  deposiwof  0"niernary  age 

Ql    I  I  iiuins.'lidalcd  marine  ictracedepotiU  of  probable  Pleistocene  3^e 
-^  n.iiiidaied  marine  thcif  and  slope  deposiu  nf  late  Pleistocene  age 

:K  ihai  may  corrcliic  with  the  San  IVdro  Formation 
KcdSanditmustiy  uncontolidsiedquarizoK  sandofPleislonne  agel. 

Red  Sanditmcstiy  unconuilidaicd  quariuiic  sand  of  Pleistocene  agei  overlain  by  ihiek 

'  ^    ^.'.f  (fisn  3m)  depcnils  ol  Q. 


1.  GEOLOGIC  CONTACT 
(buttress  unconformity) 


2.  GEOLOGIC  CONTACT 
(ponded  sediments) 


3.  GEOLOGIC  CONTACT 
(ponded  sediments) 


SedimenI  and  sedimentary  rock  of  Quaternary  and  Tertiary  (Pliocene  and  Miocene)  age. 
Teriiary  C*)  age 

and  Pleistocene  age  that  may  corrcli 


'^lidatcduniiofsund.  gravel,  etay  and  tuff  of  Pliocene  and  PlciMocene  age  that  may 

ate  with  the  1^0  Robles  Formation,  and  IS  overlain  by  thick  (greater  than  3mldc[>niitiof  Q 


I  Off       Terrace  deposiu  of  Quaternary  and 

SUnc- 
*.rb 

I     Tp    [   \tilimcniary  rockof  Phocenc  age 

fo/^j  Sclimcntary  rock  o(  Pliocene  age  overlain  by  thick  Igrcaier  than  3m)  deposiii  of  Q 

I  Tpp  I  f^J^lMma  Formation  (marine  sandstone  and  wltnone  of  Pliocene  age). 

le/T>^l  Pu'""";!  Formation  (manresandiione  and  siltsTone  of  Pliocene  age)  overlain  hyihick(t;'eaier 
r^"]   than  iml  deposits  of  Q 

I    Tpr  I  Sedimentary  rock  of  early  Pliocene  and  late  Miocene  age 

I    Tm   I  Sedimentary  rock  of  Miocene  age 

I  Q/Tm  I   Sedimentary  rock  of  Miocene  age  overlain  by  thick  (greater  than  3m)  deposits  of  Q 

I^^P  Viilunic  rock  of  Miocene  age 

I  ^"^  1  Vnltanic  and  sedimentary  nock  of  Miocene  age 

^^^1  Sania  Crui  Mudsione  (siliceoui  organic  mudiionc  of  Miocene  age) 

H  Santa  CruiMudslonel&iliceous  organic  mudstone  of  Miocene  age)  overlain  by  thick  (greater 
ihan  3m)  deposits  of  Q, 

^^H  Santa  Margariu  Formation  (sandstone  and  arkosic  sandstone  of  Miocene  age). 

IJMJIffMI  Santa  Margarita  Formation  Isandilonc  and  arkosic  sandstone  of  Miocene  age)  oveilain  by  ihick 
bBp»«1  (greater  than  3m)  deposits  of  Q 

^^^1  Monterey  Formation  (siliceous  sandstone,  silistone  and  mudstone  of  Miocene  age). 

■  Monterey  Formation  (siliceous  sandstone,  silistone  and  mudstone  of  Miocene  age)  overlaifl  by 
Ihick  (greater  Ihan  3m)  deposits  of  Q 

^^^H  Plutonic  and  hypabyssal  rock  of  Miocene  age 

^^^1  Sedimentary  rock  of  Oligoccne  age 

I    1a\   SfdimentaryrtKk  of  Eocene  age 

'  ■  i.  [iiary  rock  of  Eocene  and  Rileoccne  age 

I"  Formation  (sandstone,  tjlutone.  mudstone  and  cobble-pebble  conglomerate  of 


cage) 
1. 1  niaty  rock  of  Tertiary  age, 
ii.inic  riKk  of  Ternary  age 
Jirncniary  rock  of  late  Cretaceous  age. 


ED 

I   ^^  I  Sedimentar>' rock  of  Cretaceous  age 

^^H  Undiftereniiaicd  Igneous  rock  of  Miocene  age  and  mctamorphic  rock  of  pre-late  Cretaceous  age 


:rlhan  3m)  deposits  of  Q, 


^^H  Melamorphicrockol  pre-latcCi 

[g^  (jr.iiiiiit  rock,  chiefly  dioiile,  of  Mcsowic  age 

j    gop    I  fiirphynlicgranodjortle. 

[     jjj    j  Mcumorphiciock  of  unknown  age 

I  Q/m  ]  '^''^'■'""■'fph'c  rock  of  unknown  age  overlain  by  (hick  (grc. 

I  ffj^  I  (r.in^i«anComplM. Coastal  Belt 

^^^1  l-rjnu^anComplei,  undifferentiated 


HIGHLIGHTED  BOXES  INDICATE  UNITS  DEPICTED  ON  THIS  PLATE. 


GEOLCXjIC  CONTACT  quened  where  eon- 
■act  IS  uncertain.  All  contacts  arc  eitrapolaled 
from  scismtc-relleclion  data  and  are  approii- 
male  m  location  Eiample  from  sparker  profile 
of  upper  Tefliafy  and  Quaternary  (QTs)  sedl' 
ment,  ponded  in  ^ynclinally  folded  strata  on 
\\apt  of  pre%umed  Miocene  (Tm'')  sediments. 
LJxated  in  the  Gulf  of  Santa  Cstalma  west  of 
Dana  Pomi,  inner  southern  California  continen- 
tal borderland 


B.  FAULT 

(Pleistocene) 


GEOLOGIC  CONTACT  quined  where  contact  is  un- 
certain All  contacts  arc  e:(trap]late<l  from  seismic-rcflcc- 
lion  data  and  are  apprommattin  location  Example  from 
Uniboom  profile  of  sedimcrl  of  Quaternary  (Q)  age 
ponded  m  synclinatly  folded  ilrata  on  slope  of  Miocene 
(Tm)  sedimentary  rocks.  l.oca\ed  south  of  San  Nicolas 
Island,  middle  southern  Calfomia  continental  bonder- 


9.  FAULT 
(Tertiary) 


-  825- -^S^  __;  -."i: 


1 

1 

\ 
\ 

4  SO 

t> 

- 

i 

a 

^< 

^^ 

fl 

1^ 

\ 

" 

\ 

i 

^ 

S 

? 

I 

hi 

/ 

- 

■; 

600- 

'i 

i^ 

M 

!>._a 

67  5- 

'- 

^ 

■    ' 

_-  1 

4.  FAl 

(see 
expi 


fl 


GEOLOGIC  CONTACT  quened  where  contact  i%  unccnam 
All  contacts  arc  citrapolatcd  from  seismic -re  flee  Hon  data  and 
are  apprommate  in  location  Enomple  from  Llniboom  profile  of 
unconsolidated  Quaternary  (Q)  sediment  ponded  between  base 
of  slope  and  exposed  bedrock  171  of  probable  Miocene  (TM"") 
age  located  in  the  Gulf  of  Santa  Calahna.  inner  southern  Cal- 
ifornia conlineniol  borderland 


10.  FAULT 

(Quaternary) 


11.  FAULT 

(Quaternary  and 
Lale  Tertiary) 


i 

675- 

" 

|« 

a 

"^  i^m^^Z^r^J^ 

975- 

'        ^ 

FAULT  solid  where  well  defined,  dashed  where  inferred. 
queried  where  uncertain  Faults  designated  by  divided  txtites 
indicate  that  strata  of  late  Tertiary  and  Quaternary  age  are 
cut  Oneof  these  hasseaflooretpression,  indicated  by  bar  and 
age  symbol  on  downlhrown  side,  another  reaches  but  docs 
not  displace  seaflour.  as  indicated  by  age  symbol  nstnde  fault 
"D"  designates  downlhrown  block.  "U"  designates  up- 
thrown  block  EiampIc  from  sparker  profile  within  Loma  Sea 
Valk).  inner  southern  California  continental  borderland. 


<50- 

/^ 

■iiS- 

._:- 

/f .- 

800- 

Tm 

TP    :^ 

Tm 

V\ 

675- 

■y .- 

338- 

"1 1° 

II 

ff 

i;;  413- 

/ 

3 

z\ 

tl 

0T.|| 

4R8- 

'■•/// J 

"1 

II 

Fault  solid  where  well  Jefincd.  dashed  where  inferred, 
quened  where  uncertain  FilW  inangle  (age  symbol)  in- 
dicates youngest  strata  cm  »fe  Pliocene  (Tp)  mage  Fold- 
ed Miocene  (Tm)  sedimemary  rock  is  overlain  by 
Pliocene  strata,  both  h;  in  fault  contact  with  exposed 
t^rock  ndge  of  folded  Miocene  strata  Example  from 
sparker  profile  across  mainland  *ficlf  near  Carlsbad,  inner 
MUthem  California  cuntii""*'  borderland. 


FAULT  solid  where  well  defined,  dashed  where  in- 
ferred, queried  where  uncenain  Divided  box  ostndc 
fault  symbol  indicates  fault  does  not  have  seaftoot  ex- 
pression and  that  youngest  strata  col  are  of  late  Terti- 
ary and  Quaternary  (QTs)  age  "D"  designates 
downthrown  block.  ■'U"  designates  upthrown  block 
Fault  extends  to  base  of -'l>ubblc  pulse,"  but  apparently 
does  not  reach  the  seafloor  Note  two  unconformities 
within  strata  to  right  of  fault  Example  from  sparker 
profile  across  inner  southern  Cahfomia  conHnenlal 
borderland  near  Newport  Bcacli. 


Fault  solid  where  well  c 
where  uncertain  Open  ciri 
does  not  have  scaflooi  cxpi 
cut  arc  late  Ternary  and  (. 
fault  symbol  indicates  that 
ternary  in  age  "D"  designs 
upthrown  bicck  Fault  ui  fu 
ternary  (QTj)  ond  older  u 
Miocene  (Tm)  rocks  Esan 
across  San  Diego  shelf.  Lom 
southern  California  conline 


lA-GEORGE  DEUKMEJIAN.  GOVERNOR 

>HDON  K  VAN  VLECK,  SECRETARY  FOR  RESOURCES 

nservation-randall  m  ward,  director 


C3 


PHVSICAI  SCIENCES 
LIBRARY 

IJC  DAVIS 


CALIFORNIA  CONTINENTAL  MARGIN  GEOLOGIC  MAP  SERIES 

MASTER  LEGEND  AND  EXAMPLE  SEISMIC  REFLECTION  PROFILES 
WITH  SYMBOLS  AND  TERMINOLOGY.  (PLATE  1) 


4.  FAULT 
(seafloor 
expression) 


5.  FAULT 
(seafloor 
expression) 


6.  FAULT 
(seafloor 
expression) 


T 

■s— 

263- 

1 

M 

9 

Hi 

H 

SS^^^HjH- 

338- 

•,> 

t  ^ 

M 

^ 

*•'"* 

- 

FAULT  iolid  where  well  denned,  da&hed  where  inferred,  queried  where 
uncertain  Bar  and  a|e  symbol  «hown  on  downihrown  side  of  fauli  wiih 
•teai\<x>t  expreuion  Fnuli  displaces  jeafloor.  olTseiting  acou&iicaliy  transpar- 
cnl  unil  (QTi)  of  presumed  late  Ternary  and  Qualcmary  age  Example  from 
I  5  kKi  profile  acrcs>  inner  souihem  CalifomiD  conlinenlal  borderland  near 
San  Diego 


FAULT  solid  where  well  defined,  dashed  where  mferred,  qucned 
where  uncertain  Bar  and  age  symbol  shown  on  downlhrown  side  of 
fault  ihal  hu  seaFtoor  expression  Fault  displaces  seafloor.  offsetring 
sediments  of  presumed  laie  Tertiary  and  Quaternary  (QTs)  age  and 
juntaposmg  subjaceni  units  of  Miocene  (Tin)  and  possibly  Pliocene 
[Tp**)  ages  Also  nolc inferred  fault  wilhin  probable  Miocene  section, 
and  folded  siraia  Example  from  Uniboom  profile  across  Tanner  Bank, 
middle  southern  California  continental  borderland  (after  Greene  and 
Olhen.  1975,  Iheir  Figure  3) 


J ,- 


FAULT  solid  where  well  defined,  dashed  where  inferred,  queried 
where  uncertain  Bar  and  age  symbol  shown  on  downlhrown  side  of 
fault  that  has  seafloor  enpreuion.  Fauli  displaces  seafloor.  oflsetiing 
units  of  laie  Tertiary  amd  Quaternary  (QTs)  age  and  juilaposing 
subjacent  units  of  probable  Miocene  (Tm?)  age  Example  from  ^rkcr 
profile  across  mainland  shelf,  inner  southern  Califomli  continental 
borderland  near  Occanside 


FAULT  solid  where  well  defined,  dashed  where  inferred,  que- 
ried where  uncenain  Bar  and  age  symbol  shown  on  down- 
lhrown side  of  fault  that  has  leafloor  cxpreuion  Divided  boi 
indicates  youngest  strata  cut  are  of  Quaternary  age  Note  thai 
one  questionable  and  four  inferred  faults  cutting  Miocene  (Tm?) 
or  older  strata  arc  indicated  by  open  mangles  asindc  fault  sym- 
bol "D"  designates  downlhrown  block,  "U"  designates  up- 
thrown  block  These  strata  are  also  folded,  as  shown  by  anticline 
and  syncline  symbols  Eumple  from  sparker  profile  across  Gulf 
of  Sania  Caialina.  inner  southern  California  conlinental  border- 
land. 


15.  FAULT  ZONE 


0- 

.  ,  1 

J-° 

n 

1 

P 

If 

1 

-  -0,i 

1            250- 

HHv 

-i 

!   lii! 

-  \ 

' 

':    'K'.'?'?^' 

W    i'i^.ifr 

A  - 

J 

!"!■' 

&0i  - 

i.      ..-J    .... 

;:::;^l:; 

'            :'lM'^ 

m-A:^, 

fMi^kl-ii., 

■nw 

i/jh 

■-ii^,„ 

FAULT  uhd  where  well  defmcd.  dashed  where  inferred,  queried 
where  uncertain.  Open  circle  astnde  fault  symbol  indicates  fault 
does  noi  hive  seafloor  eiprcssiun  and  (hat  youngest  strata  (QTs| 
cut  are  lait  Tertiary  and  Qualemary  in  age  Divided  bo»  asinde 
fault  symbol  rndicaics  that  the  strata  cul  ate  undiffercntialed  Qua- 
ternary m  tge.  "D"  designates  downlhrown  block,  "U"  designates 
upihrown block  Fault  at  far  left  junlaposei  laie  Ternary  and  Qua- 
lemary (QTs)  and  older  units  with  an  exposed  bedrock  ndgc  of 
Miocene  (Tm  I  rocks.  Biample  of  fauli  ion e  from  Uniboom  profile 
across  San  Diego  shelf,  Loma  Sea  Valley,  and  Coronado  Bank,  inner 
southern  California  continental  borderland. 


FAULT  solid  where  well  defined,  dashed  where  in- 
ferred, qucned  where  uncertain  Open  circles  asinde 
fault  symbol  indicates  faults  do  not  have  seafloor  ex- 
pression and  youngcsi  slrala  cul  arc  late  Tertiary  and 
Quaternary  IQTs)  in  age  "D"  designates  down- 
lhrown block,  "U"  designates  upihrown  block  Where 
faults  are  close  logclher,  they  arc  sometimes  mapped 
asoFAULTZONE  (see  Example  15)  Nole  that  fault 
at  left  juxtaposes  laie  Tertiary  and  Qualemary  siraia 
wnh  an  exposed  bedrock  block  of  Miocene  (Tm)  age 
Example  from  sparker  profile  across  San  Diego  shelf. 
Loma  Sea  Valley,  and  cast  flank  of  Coronado  Bank, 
inner  southern  California  continental  borderland. 


FAULT  solid  where  well  defined,  dashed  where  inferred,  que- 
ried where  uncertain  Open  tnangle  asinde  fault  symbol  indi- 
cates fault  does  not  have  seafloor  expression  and  strata  cut  are 
probably  Miocene  (Tm?)  in  age  "D"  designates  downlhrown 
block;  "U"  designates  upihrown  block  Nole  also  the  two  faults 
at  Ihe  fat  nght  that  are  designated  by  filled  box  and  bar  on  the 
fault  symbol  These  have  scaHoor  expression,  and  cul  slrota  of 
presumed  Holocene  age.  Example  from  sparker  profile  across 
San  Diego  shelf  to  Lama  Sea  Valley,  inner  soulhem  Califomis 
continental  borderland 


Fault  Uhrusil  solid  where  well  defined,  dashed  where 
inferred,  quened  where  uncertain  Barbs  are  shown  on 
upper  plate  Note  thai  the  youngeil  H'a'a  cut  are  of  late 
Ternary  and  Qualcmary  (QTs)  age  Example  from  spark- 
er profile  across  shelf  west  of  Veniurt.  middle  southern 
California  continental  borderland  lal"  Greene  and  oth- 
er*, 1978,  their  Plate  1) 


T      r 


FAULT  ZONE  solid  where  well  defined,  dashed  where  in- 
ferred, queried  where  uncertain  Fault  lonc  oFTsels  sedimentary 
rocks  of  Miocene  (Tm)  age  and  locally  may  extend  lo  ihe  sea- 
floor Example  from  the  sparker  profile  across  shelf  south  of  San 
Mateo  Point,  inner  souihem  California  continental  borderland 
(after  Greene  uiil  Kennedy.  1481 ) 


touiTiEm  CaliromiB  conlintnial  borderlind. 


bedrtKk  ndge  of  folded  Mioccni  ilrata  Ew 
iparker  profile  acrou  nil'Nani]  ihtlf  near  Car 
uiulhcm  CalifomiB  conli'Bn>«l  *orJ«'l»B<l 


etland  near  New 


I  conunenial 


'i-     ij^                    1   >}t-                         /?^.                        t^o- 

^  ) 

/    3d7[r^~~~~~~~..^^ 

1    *'*^  /          ~^~~~~^ 

1     *  //     "         / 

-  C  (7    .       / 

'r-. 

: Tt?  ^      / 

T  /    J  /  ~ 

( 

\ 

3S-- 

\ 

\ 

/   K  / ' 

w     /        ?    / 

/ 

tV 

n 

^j- 

r?^                                 yo-                               "8*                      \       '/6' 

32V 

16.  FAULTED  ANTICLINE 


17.  FOLD 

(anilcllne) 


LOCATION  MAP  OF  PROFILE  EXAMPLES 

Index  mop  showing  locaUoiuofieumic-rEncction  exampla.  Locaiioiuorejumplesarcapprau- 
male  and  the  erfiion  may  be  coniacied  for  more  informHiion,  Tlic  circle  and  number  five 
approumaie  locslion  of  the  seismic  line  and  the  line  within  the  circle  U  aligned  in  the  ume 
direclionBt  Ihcuismic  trackline  Example  I9isiepreseiiledby  alinconly  Examples  spaced  c>i»c 
togelherarcplollcd  uilhin  iJie  same  circle  as  one  tine,  i.e..  1,10.  Examples  which  are  on  Iheumc 
line  hut  at  difTcrenl  tholpointi  are  shown  with  two  crossbars  on  the  line  inside  (he  circle,  i.e.  S.H 


16.  FOLD 
(antlcllna. 
syncllne) 


^1500 
22S0 


FAULTED  ANTICLINE  Gai  migrating 
upward  along  faults  in  late  Tertiary  and  Qua- 
ternary (QTs)  siraia  has  accumulated  along 
the  faulted  aniiclmal  crest,  increasing  the 
acoustic  contrast  Example  from  !-scc,  sin- 
gle-channel airgun  reflection  record  m  off- 
shore Santa  Mana  basin,  south  central 
Califomia  continental  margin 


FOLD  <aniicline)i  axis  shown  ai  solid  line  where  well 
defined,  dashed  where  inferred,  queried  where  uncertain- 
Arrow  indicates  direction  of  axial  plunge.  Also  note  small 
gynclme  to  nght  of  anticline,  and  angular  unconformity 
between  undifFcrcn Mated  igneous  ind  sedimentary  rocks 
of  probable  Miocene  age  (Tmu?),»nd  overlying  strata  of 
Miocene  (Tml  age  Example  l:om  Uniboom  profile 
between  the  Tanner  and  Cortes  Binks,  middle  southern 
California  continental  borderland. 


5- 

1 

0- 

1 

Tm       1   Tm 

1 

s-  ^  ^ 

zw 

I'-y^^ 

1 

-H 


FOLD  (aniiclinc)  aiis  shown  as  solid  line  where  well  defined,  dashed 
where  inferred,  quened  where  uncertain  Arrow  indicates  direction  of 
axial  plunge  Also  note  imall  syncline  located  between  the  two  anticlinal 
folds,  and  the  angular  unconformity  between  folded  strata  of  Miocene 
(Tm)  age  and  the  progradational  sequence  of  Miocene  (Tm)  sedimentary 
rocks.  Example  from  Uniboom  profile  across  San  Nicolas  Island  platform. 
middle  southern  California  coniinenial  borderland 


KEY  TO  RECENCY  OF  FAULTING 
FAULTS 

Sohd  where  well  denned,  dashed  where  inferred,  queried  where  uncertain. 
Barbs  shown  on  upper  plate  of  thruM  fault.  Where  fault  olTsels  sea  floor,  age  symbol  is  shown 
on  bar  on  downthrown  vide.  Where  age  was  determined,  age  symbol  is  shown  astride  fault  and 
relative  olTset  is  shown  by  "D"  and  "0"on  downthrown  and  upihrown  tides  Ages  of  faults  are 
indicated  as  follows,  all  faults  considered  active  or  poientiatty  uclivc  shown  in  red: 
S        cuts  strata  of  Holoccne  age 
Q         cuts  strata  of  Pleiilocene  age 
g        cuts  strata  of  Quaternary  age 
O  (ul*  slrala  of  late  Tertiary  and  Quflternary   age 

A  cuts  strata  of  Pliocene  age 
t^  cuts  Miocene  or  older  strata 

7 ^ A  ;   a 


23.  CHANNEL 
llllledl 


24.  CHANNEL 
llllleil) 


2S.  CHANNEL 
(buriad) 


338- 

g 

W/W/Z/M 

tt 

S!413- 

— 

X 

-<;:7-     —        qT5      -' —  -  =- — ^^--,.;^ 

^^  -=— ^T'    _  .^SSS^:^^ 

488- 

QTs                           '"""  ■                                    0T» 

CHANNEL  (filled)  dash-dot  line  marks  paleochannci  axis,  arrow 
indicates  direction  ofsedimenl  transport  Channel  margins  indicat- 
ed by  solid  line  where  well  defined,  dashed  where  inferred,  queried 
where  uncertain  Example  from  Uniboom  profileof  upper  Ternary 
and  Quaternary  IQTs)  sediments  filling  an  erosionul  channel  locat- 
ed ofT  Point  La  Jolla.  inner  southern  California  continental  border- 
land. 


^^as3 


CHANNEL  (filled)  dash-dot  line  marks  paleochennel  axis  [not  located  on 
profile  ;4>ove).  arrow  indicates  direction  ofsedimenl  transport  Channel  margins 
indicated  by  solid  line  where  well  defined,  dashed  where  inferred,  queried  where 
uncertan  Note  that  old  channel  deposits  (QcO  have  been  incised  by  subsequent 
erosion,  rcsulimg  in  the  formation  of  a  modem,  active  channel  Symbols.  QTv 
upper  Ttniary  and  Quaternary  sediments:  Tpp*",  Pliocene  Punsima  C)  Forma' 
lion  Eximple  from  Uniboom  profile  across  Ascension  Canyon,  central  Califor- 
nia contrienial  margin 


CHANNEL  (buned)  duh-dot  line  marks  p; 
row  indicates  direction  of  sediment  irsnspor 
indicated  by  dotted  line  Also  note  Ihechannel  t 
to  the  left  of  buned  channel,  filled  wilh  undifli 
of  late  Ternary  and  QuaiemBry  ((jTs)  age. 
occupying  the  site  of  this  older,  filled  channel  < 
the  presence  of  low-relief  erosional  warps  at  il 
from  sparker  profile  aerots  the  Gulf  of  Santa 
Point,  inner  southern  Calilorma  continental  b 


^^.rfS«C»i 


i?^-^^S 


30.  LANDSLIDE 
(slump) 


31.  LANDSLIDE 
'B'ump) 


32.  LANDSLIDE 
(slump) 


.  LANDSLIDE  (7) 
(■lump)  (7  > 


34.  LANDSLIDE 
(scarps) 


19.  STRUCTURAL  HIGH  AND  LOW 


20.  STRUCTURAL  HIqh 


21.  CHANNEL 
(active) 


22.  CHANNEL 
(filled  I 


^,,1J«W|I!I|||| 


KfLOMETERS 

«J=> 

^ 

QTt 

'SO- 

_     -atT^ 

j^^^l 

t^BibL[~ 

1500- 

^^^^^^M 

^^-           Ts7 

/ 

2Z%0- 

i^ 

.  j- 

- 

— 

~i 

—^ 

— 

-T- 

^-- 

- 

, 

. 

__ 

, 

^ 

? 

=^ 

— 

^ 

r  - 

q 

25- 

li 

k' 

^ 

-0,7 

^-  f'^ 

-J 

"J  I 

— 

^}^ 

r 

.__ 

00- 

-0.8 

,^ 

■^ 

*^ 

i^ 

— 

'_ 

V 

1—- 

__. 

T^ 

~ 

^tr 

— 

n 

■  -- 

-^ 

^— 

— ■ 

k- 

— 

^ 

■■ — 

"■ 

. 

i.. 

„ 

_.. 

STRUCTURAL  HIGHS  AND  LOWS:  solid  whcfc  well  defmed.  daihed 
where  inferred,  quened  where  unccnain  Struclural  highs  formed  by  ihe 
Farallon  Ridge  ICrelaceous  grannie  rocks,  gr,  of  rhc  Salinian  lerrane  of 
Silberling  and  others.  1984)  and  Ihe  Sanla  Cruz  high  (Crelaceoussubduclion 
melange  of  Franciscan  Complex.  KJfj  and  ihc  mrervcning  struclural  low 
filled  by  Ihe  laie  Tertiary  and  Qualcmary  scdimcnls  of  the  outer  Sanla  Cruz 
iwMn  Line  drawing  from  a  4-second.  single-channel  sparker  profile  run 
across  Iheconlinenlalsheirand  slope  wcsl  ofHalfMoon  Bay.olTshorecenlral 
California. 


-4- 


0  O.S  1-0  1,S 

I I I  I 

KILOMETERS 


CHANNEL  (aclive)  dosh-dol  tine  marks  channel  aMi.  arrow  indicalcs 
direcMon  of  sediment  iransporl.  Also  nole  Iwo  buned  channels  beneath  the 
modem  sea  floor  of  presumed  Quale  mary- Ternary,  undifTerenliaied  age  to 
nght  of  active  channels  Enamplc  from  sparker  profile  acroa  head  of 
Arguello  Canyon,  off  Pomt  Arguello,  central  California  conimcmal  mar- 
gin 


STRUCTURAL  HIGH  solid  where  well  defined,  dashed  where  inferred, 
queried  where  uncerbin  Top  of  struclural  high  is  surface  eroded  onto 
presumed  sedimentaiy  rocks  (Ts)  of  Tertiary  age  buned  beneath  undif- 
ferentiated sedimentary  rocks  and  sediments  (QTs)  of  Tertiary  and  Qua- 
ternary age.  EnampV  from  sparker  prolilc  acrosi  the  Gulf  of  Sanla 
CsTslina. 


CHANNEL  irillcd)  duh-dol  hne  mafks  palcochannel  aus. 
arrow  indicates  direction  of  ledimem  iranipon  Channel  mar- 
gins indicated  by  w>lid  tine  where  well  defined,  dashed  where 
inferred,  queried  where  uncenain  Also  note  faull  (hat  culs  (lai- 
lying  sediments  of  presumed  Holoccne  age  and  is  expressed  m 
Ihe  seadoor  Example  from  Uniboom  profile  off  Point  Ano 
Nuevo.  central  California  contmenial  margin 


-^- 


iZ-l'Z£ 


26.  CHANNEL 

(burled) 


26.  LANDSLIDE 

(creep) 


29.  LANDSLIDE 

(Slump) 


KILOMETERS 


'  dash-doi  line  marks  paleochannel  axis,  ar- 
an  of  sedimtnt  iranspon  Channel  margins 
ic  Also  nole  ihc  channel  al  lurfagc,  above  and 
hannel.  filled  with  undilTcrenliated  ledi 
Quaternary  (QTs)  age  A  modem  channel 
this  older,  filled  channel  may  l>e  mdicaled  by 
:lief  erosion  al  warps  al  Ihe  surface  Example 
across  the  Gulf  of  Santa  Caialina.  olT  Dana 
Califomia  continental  borderland. 


4  50- 

A:   \U\  _ 

^-— V---_  ~  £:'!  2'yv_—=^r^ 

;f  =?^  -  -"l^-'^^jji^j: 

060- 

f^^-fi^^Vfr- 


CHANNEL  (buned)  dash-doi  line  marks  paleo- 
channel axis  (not  indicated  on  profile  above). 
Wiihm  upper  Tertiary  and  Quaternary  (QTs)  sedi- 
ments, the  channel  margins  are  indicated  by  doited 
lines  Pulled-down  reflccton,  immediately  beneath 
ihechanncland  incoherent  reflectors  at  depth  prob- 
ably result  from  low  acouslic  velocities  auoaaied 
with  unconsolidated  channel  fill  materials  Exam- 
ple from  sparker  profile  across  the  Gulf  of  Sanla 
Catalma,  inner  southern  California  contmenial  bor- 
derland 


LEVEE  solid  where  well  defined,  duhcd 
Hherc  inferred,  queried  where  uncertain 
Levees  constructed  from  sediment  overflow 
tractive  submanne  channel  (shown  as  dash- 
dol  line  with  arrow  indicating  direction  of 
ledimenl  transport)  Levees  of  Quaternary 
Ige  are  deposited  upon  flat  lying  sirala  of 
ledimenti  and  sedimentary  rocks  of  Qualer- 
»ary  and  Tertiary,  undilTerentiatcd.  age 
(QTs)  Example  from  sparker  profile  across 
door  of  Gulf  of  Santa  Catalma  at  base  of 
ilope  west  of  San  Maieo  Point,  southern  Cali- 
fornia continental  borderland. 


CREEP  [noted  on  a  imgte  survey  line):  arrow  mdicales  apparent  direc- 
tion of  sediment  movement  in  upper  Ternary  and  Quaternary  (QTs) 
sediments  Example  from  Uniboom  profile  off  Oceans  id  e.  inner  southern 
California  conlinental  borderland 


SLUMP  boundanes  solid  where  well  defined,  dashed  where 
inferred,  queried  where  uncertain  Arrows  indicate  direction  of 
movement  Zone  of  movement  extends  to  a  subboiiom  depth  of 
approximately  20  m  Note  hummocky  seaHoor  surface  and  back- 
rt)taied  subboiiom  refleciore  (slip  surface)  Example  from  Uni- 
boom profile  across  contmenial  slope  off  Crescent  City,  northern 
Califomia  continental  margin 


4NDSL(0E 

carps) 


35.  LANDSLIDE 
(block  glide) 


36.  LANDSLIDE 
(block  glide) 


37.  LANDSLIDE 
(sediment  flow) 


38.  QAS 

(seep) 
375-| 


3.  LANDSLIDE  <7) 
(tlumpX?) 


34.  LANDSLIDE 
(scarps) 


**^'*^^W;! 


0 

-,-: 

1 

Sfii 

0.05 

g     4SO-       ,            ,        ^ 
0.10O 

^':&  ^B 

1 

"'"  % 

■  -'^n 

0.20 

600- 

ss^l^ 

■ 

675- 

: 

! 

SLIIMP   boundano  wMd  where  *cll  dcHncd.  diihed  whcfe  infefted,  queried 

where  unccrlain    Arrowt  indiL-alc  dtreclion  oS  movemeni    Zone  or 

eilends  to  3  subbollom  depth  of  JO  m    Noie  hummocliy  «afl«>r  surface,  ilip 

surfsco  and  back  rotation  of  renecton  wilhin  moving  Kdimi 

from  Unibootn  profile  acnn»  ilope  wcsl-nonhwni  of  Cmcertt  Cily.  r)Dnhem 

CaliromiB  coniinenlal  murgin  ufier  Field  and  others  I9B0.  iheir  Figure  IS) 


1 

.,^- 

^ 

^^s>s^^^--^^                         ~ 

~~"^^^^^^^=      -""IT  —  -^^^i^^^?^ 

--,,.,^ 

55->-^ 

—   ^ 

SLUMP  boundaries  solid  where  well  defined,  dashed  where 
inftfTed,  quened  where  oneenain  Arrows  indieaie  di  reel  ion 
of  rnovemenl  Zone  of  movement  extends  lo  a  tubboltom 
depth  of  in  excess  of  100  m  involving  sediments  of  lale  Terti- 
an, and  Qua  ternary  (QTs)  age  Note  slip  surfaces  and  appsf- 
eni  drag  folding  of  strata  adjacent  to  slip  iurfaces  Example 
from  Umboom  profile  near  [-a  Jolla  Canyon,  inner  souihem 
California  continental  borderland. 


SLUMP  boundaries  solid  where  well  dcrincd.  dashed  where  inferred, 
quened  where  uncertain  Arrows  indicate  direction  of  movemtnl  Zoneof 
movement  extends  to  a  subbotiom  depth  of  approximately  °0  m  in  sedi' 
ments  of  lale  Tertiary  and  Quutcmary  (QTsl  age  Note  apparent  slip 
surfaces  and  back-rotated  reflectors  Example  from  Unboom  profile 
across  Ascension  Canyon,  central  Califomia  cotttmenlal  lutgm. 


SLUMP  bnundnnes  solid  where  well  dcrined.  dashed  where  inferred, 
quened  where  uncermm  Arrows  indicate  apparent  direction  of  move- 
deposits  oriaic  Tertiary  and  Quaternary  (QTs)  age  Movemeni 
of  the  slump  mass  along  a  generally  arcuate  failure  surface  has  de- 
stroyed the  bedding  and  produced  a  nonrcflccling  tone  Example  from 
Umboom  profile  across  the  continental  slope  ofT  outer  Santa  Cruz  basin, 
central  California  continental  margin 


GAS  area  of  acoustic  anomaly  possibl>  indicating  the  prcsenic  of  gas- 
saturated  sediments.  Solid  where  well  defined  dashed  where  inferred 
quened  where  uncenam  AiouMit  anomalies  above  occur  in  flat  lying 
Quaternary  (Q)  sediment  overlying  an  eroded  flat  lopped  Miocene 
(Tm)  ticdrock  ndge  Example  from  Unihoom  profile  across  San  Pedro 
escarpment  and  ihelf.  middle  uiulhem  California  continental  borderland 


GAS:  area  of  acouslit  anomaly,  possibly  indicating  the  presence  of 
gas-saturated  sediment  Solid  where  well  defined,  dashed  where 
inferred,  quened  where  uncertain.  Example  from  Umboom  profile 
acrossshelfandupper  slope  west  of  Crescent  City,  northern  Califor- 
nia continental  margin. 


SCARPS  houndanes  solid  whe 
quened  where  unt 
movement  invalves  sediment  ofl 
age.  Note  double  hachurts  ind{ 
Uniboom  profile  across  La  Jol| 
i»)nlinental  borderland. 


GAS  area  of  acoustic  anomaly,  possibly  indicating  the  presence  of  gas  saturated 
sediment  Solid  where  w^ll  defined,  dashed  where  inferred,  quened  where  uncertain 
Example  from  )  5  kHi  profile  ocross  shelf  off  Crocent  City,  riorthem  Califomio 
continental  margin 


DIAPIRIC  RIDGE  Solid  where  well  defined,  dashed  where  inferred, 
quened  where  uncertain  Shale-cored  diapir  pierces  upper  Ternary  and 
Quaternary  (QTs)  strata  and  extends  above  the  seafloor  Example  from 
.1  S  kHi  profile  across  marginal  plateau  west-northwest  of  Eureka,  north- 
ern California  continental  margin 


•US  Geological  Survey 
"California  Deparimcm  of  Conservation.  Diviii 
Scripps  Insiiiuiion  of  Oceanography 


D  of  Mines  and  Geology. 


MASTER   LEGEND   AND   EXAMPLE 
PROFILES    WITH    SYMBOLS  A] 

H.  GARY  GREENE*  AND  MICHAEL  P.  I 


^^/V^-^I 


37.  LANOSLIOE 
(sadlmcnt  flow) 


S  boundjnts  m-IiJ  where  well  defined,  diuhcd  where  inferred, 
where  unieriBin  Hachutes  mditaic  slump  scarp  Zone  of 
nf  involvi^  icdimcnl  of  late  Ternary  and  Qualernary  (QTs) 
tc  double  hathurCT  indicaic  eroiional  wnrpi  Eumpk  from 
n  profile  jtri»t  La  Jolla  Canyon,  inner  voulhcm  California 
Inl  borderland 


BLOCK  GLIDE  boundsnes  wlid  where  well  defined,  disM  where 
inferred,  quened  where  uncertain  Arrows  indicate  apparenl  diieclion  of 
movemeni  Zone  of  movemcnl  e«iends  lo  a  subbotlom  depth  rf  150-190 
m.  involving  udimcnts  of  laie  Ter1iaf>  and  Qualemar>  (OTs)  tge  Noie 
relative  acouslic  transparency  of  blocks,  possibly  the  result  of  in 
deformalion  of  strata  within  the  blocks  Erosional  channelt  maj  develop 
locally  along  pull-apan  fracture*  between  blocks,  shown  by  doolie  hac- 
hurc*  (erosional  scarp)  Example  from  sparker  profile  across  base  ofslope 
off  Newport  Beach,  inner  southern  California  continental  bordcrla»d  (aft- 
e  and  others  I98J.  their  Figure  MO) 


BLOCK  GLIDE,  boundancs sohd  wher 
dashed  where  inferred,  quened  where  u 
rows  indicate  apparenl  direction  of  movemeni  Zone  of 
movement  extends  lo  a  subbotiom  depth  of  approxi- 
mately 90-100  m.  involving  sediments  of  laie  Tertiary 
and  Quaternary  IQTs)  age  Note  that  internal  defor- 
mation of  blocks  IS  greatest  toward  the  from  edge 
(downslopc).  and  sole  (basel  of  the  mass.  Locally 
erosional  channels  may  develop  along  pull-apan  frac- 
tures between  the  blocks  These  are  shown  with  double 
hachures  (erosional  scarp)  Example  from  mini-spark- 
er  profile  across  slope  south  of  Newport  Beach,  inner 
southern  California  continental  borderland 


SEDIMENT  FLOW  Boundaries  solid  where  well  defined,  dashed 
where  inferred,  quened  where  uncertain  Arrows  indicate  direction 
of  movemeni  in  sediments  of  late  Tertury  jnd  Quaiemiiry  (QTs) 
age  Note  multiple  headscarps  above  thick,  detached  sediment  mass, 
acoustic  transparency  of  this  mass,  and  absence  of  an  identifiable 
slip  surface  Enample  from  Uniboom  profile  across  north  slope  of 
Santa  Barbara  Channel,  (approwmaiely  JS  1 
bara  (from  Edwards,  1982) 


f:i.%y;-Jv) 


)  west  of  Santa  Bar- 


OIL  AND/OR  GAS  SEEP  vymbol  indicates  presence 
of  subbotiom  and  water  column  acoustic  anomalies 
associated  with  gass.rps  Gasscepoccun  in  sediments 
of  late  Ternary  and  Quaternary  (QTs)  age  Queried 
where  uncertain  E.iamplc  from  Uniboom  profile 
across  base  of  slope  off  Point  La  Jolla,  inner  southern 
Cahfomia  continental  borderland  (after  Greene  and 
others,  1983,  their  Figure  2-16) 


44.  TERRACE 

(constructional) 


45.  TERRACE 
(erosional) 


46.  TERRACE 

(aroslonal) 


f^ 


!S 


DIAPIRIC  RIDGE  Solid  where  well  defined,  da^thed  where 
inferred,  quened  where  uncertain  Shale<orcd  diapir  pierces 
upper  Ternary  and  Quaternary  IQTs)  and  older  strata  and 
extends  above  the  seaFlocr  Example  from  sparker  pronte 
across  margmal  plateau  wcst-northwesl  of  Eureka,  northern 
California  continental  margin. 


TERRACE  (constructionjll  Ewmple  from  Uniboom  profile 
across  east  flank  of  Cones  Bank,  middle  wuthern  California  conti- 
nental borderland,  showing  Pleistocene  (QTl  pt.^gradational  ter- 
race sequences  forming  a  caistructionjl  <"  dep.>sitionul  manne 
(errace  (after  Greene  and  oilier*.  lOlJ.  their  Figure  5) 


TERRACE  (ermionall  Example  from  Uniboom  profile  atr 
off  Point  La  Jolla.  inner  southern  California  continental  borderland 
Undifferentiaied.  folded  Cretaceous  strata  (Kul  and  overlying  upper 
Ternary  and  Quaternary  (QTs)  progredai tonal  M^uence  have  bccti 
bevelled  by  wave  action  Acoustically  trantparant  unit  overlying  *•*<• 
cut  platform  is  probably  Holocene  <Q)  in  age 


TERRACE  (erosional!  Wave-planed,  platform  composed  of  undifferentiated. 
folded  Cretace«u»  ( Ku)  strata,  forming  a  wave-cut  terrace,  parnally  overlain  by 
acoustically  rraniparani  layer  of  Holocene  (Ql  age  Example  from  Unibootn 
profile  across  thelf  off  Point  La  Jolla.  inner  southern  California  continental 
borderland  (after  Greene  and  others,  198),  their  Figure  2-18) 


EXAMPLE   SEISMIC  REFLECTION 
MBOLS  AND  TERMINOLOGY. 

)  MICHAEL  P.  KENNEDY**,  EDITORS 


DIVISION  OF  MINES  AND  GEOLOGY 
JAMES  F   DAVIS,  STATE  GEOLOGIST 


STATE  OF  CALIFORNIA-GEORGE  DEUKMEJIAN  ,  GOVERNOR 

THE  RESOURCES  AGENCr- GORDON  K    VAN  VLECK,  SECRETARY  FOR  RESOURCES 
DEPARTMENT  OF  CONSERVATION  -  DON  L    BLUBAUGH,  DIRECTOR 


1908 


MAP  A:  Foults  shown  on  the  first  fault  mop  of  California,  From  Mop  No.  I  of  the  Stoto  Eorlhquahe  Investigotron  Commission 
report  on  the  Californio  eoflhquoke  of  April  18,  1906  (Lowsor>,  and  others,  1908),  Fault  nomes  shown  in  quotation 
merits  ore  from  tent  of   1908  report;  other  fogit  names  were  added  from  current  usage. 


1916 


MAP  e,  H.O.  Wood'!  (19161  abridg.d  v.riion  o)  lowioni  1908  (oull  mop  of  Colifornio,  ihowmg  loulii  or.d  "lines-  tentotiv.ly 
considered  by  Wood  lo  be  generatrices  of  eorthquokes. 


EXPLANATION 


San  Andreas  rauit 

a)  Punta  Gorda-foinl  Arena  segment 

b)  Pan)  Arena-San  Juan  segment 
C|     San  Juan-Te|on  sogmoni 

d)     Teion-CoiOfaOo  segmeni 

Cureka-Uiuah-San  Pablo  hne 

MounI  5L  Helens  faun 

Swsun  fault  (now  c«Ilsd  Green  Valley  fault) 

Mare  isiarxi-Nevsda-Carson  line 

Ha ywards  fault  mo*  Haifward  laud) 

Sunol  fault  system  (also  known  as  Calaweras  t« 

San  Gtegono  fault 

Monleiey  submanne  fauH-iono 

Pataro  faufi 

Groal  Valley  ana 

a)  Shasta -Stockton  sag  mem 

b)  Stockton- Tofucfiapi  ^egmont 
Honey  lake  taoll-ione 

jmbw*d.  but  M*fltifi«d.  laulti  br  Woods  Klomoiti  Loha 


13.  Swrra  lault  system 

a)    Beckwitti-Mono  segment 
D)    Mono-Tejoo  tegmenl 

14.  sonlB  Luoa  lautl 
Lockwood  fault 

15.  Templaton  fault 

lt    San  Un  Obnpo  'aull  (now  part  of  Nacmuento  faurt-z< 
17     Kern  fault  (now  Kem  Canyon  faulll 
te    Santa  Vnez  fault 

19  San  Gabnel  tault 

20  Santa  Monica  fault 

2^     San  Pedro  submanne  fault -iotm 
22    WNttw  fault 

23.  Santa  Ana  tault 

24.  Elvnore  fault 
Agu*  Callenle  fault 

hJortti.  and  South  Canio  l«*ct  fault 
25      San  j«£ttilo  fault 


iihwll  liho-W^  *•<>' 


■(  Mounloint  foulll,  Bed*  toutt. 


Fault  and  Geologic  Data  Maps  of  CoMfornia 
BULLETIN    201,    PLATE    I 


1922 


ucc 


EXPLANATION 


1.  Burden  Mtn.  F. 

2.  ChJco  monocline  F. 

3.  Chino  F 

4.  Coyote  Creek  F 

5.  Cristianitos  F, 

6.  Cucamonga  F 

7.  Dry  Creek  fault 

8.  Faults  in  Anderson  Valley  and  Navarro  R, 

9.  Fault  (n  Capay  Valley 

10.  Fault  al  Diablo  Canyon 

11.  Fault  by  Dunnigan  Hills 

12.  Fault  in  Palm  Canyon 

13.  Fault  along  San  Antonio  Creek 

14.  Fault  at  San  Simeon 

15.  Fault  on  W.  side  Panaminl  Va. 

16.  Faull  on  W.  side  Saline  Va. 
17  Johnson  Va.  F. 

18-  Kern  Gorge  F 

19.  Liebre-Clean*ater  F 

20.  bttle  Pine  F 

21.  No.  Branch  San  Andreas  F. 

22.  Oakndge-Santa  Susana  F 

23.  Old  Womar>  Spnngs  F, 

24.  Palos  Verdes  F 

25.  Pipes  Canyon  F 

26  Rinconada  F 

27  Rogers  Creek'Healdsburg  F. 

28  San  Fernando  F, 

29  San  Francisqulto  F. 

30.  San  Gabnel  F, 

31.  San  Gabriel  F, 

32.  Sien-a  Madre  F, 

33-  Tolay  F 

34-  Tularcitos  F, 


LEGEND 


ACTIVE  FAULT,  well  located 
ACTIVE  FAULT,  uncertainly  located 
PROBABLY  ACTIVE  FAULT 
DEAD  FAULT,  well  located 
DEAD  FAULT,  uncertainly  located 
PROBABLE  FAULT,  localionand 
character  uncertain 


MAP  C:  Faults  shown  on  the  Fault  Map  of  California  compiled  by  B.  Willis  and  H.O.  Wood  and  published  by  the  Seis- 
mologicol  Society  of  America  in  1922  at  a  scale  of  1:506,880.  Faults  were  not  shown  by  nome  on  the  original 
map,  but  have  been  identified  on  this  plote. 


1947 


LEGEND 

MAJOR  FAULTS,  well  located 
MAJOR  FAULTS,  approximately  located 
OTHER  FAULTS,  well  located 
OTHER  FAULTS,  approximately  located 
FAULT  LOCATION,  uncertain 


MAP  E:  Foult  map  of  southern  California  (here  slightly  generalized)  compiled  by  H.O.  Wood.  Faults  wetp  taken  largely  from 
the  1922  Fault  Mop  of  California  and  the  1938  Geologic  Mop  of  California.  This  foult  mop  (with  epicenters)  was 
published  in  the  Bulletin  of  Seismological  Society  of  America,  July  1947. 


1938 


Faults  of  Lake  Tahoe  graben  (Lindgren,  1887,  USGS  Folio) 

Concord 

Coasi  Ridge 

Rinconada  (part) 

Nacimrenio 

Owens  Valley  (v  mcomp'ele  -  only  pari  that  broke  at  Lone  Pme) 

Sietra  Nevada  (v  incomplele) 

San  Gabriel  (disappearing  under  Frazier  thrusi) 

Clearwaler 

Arroyo  Panda  (part) 

San  Cayelano 

San  Gabnel  (eastern  end) 

Sierra  Madre 

Raymond 

Cucamonga 

Newpon-lnglewood 

Rose  Canyon 


MAP  D:  Faults  shown  on  the  Geologic  Mop  of  California  published  in  1938  ot  1:500,000  scale.  This  reduced  version,  showing 
faults  only,  includes  oil  those  faults  shown  on  the  larger  scale  mop,  Foults  were  not  shown  by  name  on  the  original 
map,  but  have  been  identified  on  this  plate. 


yM 


^