DCL-14-081, Diablo Canyon Units 1 and 2, Central Coastal California Seismic Imaging Project (Cccsip) Chapter 7, GEO.DCPP.TR.14.03 R0 Figures 09-05-14
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File path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_1-01.mxd; Date: 06/17/2014; User: Alex Remar, LCI!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!
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_Irish Hillsstudy area150112/140107101113114102206115103-104204123207117118121128138-149105702141-1422011 3DVolumeMorroBayEsteroBaySan LuisBayCoast RangesEdna HillsIrish Hills Los Osos ValleySan Luis Obispo Creek S T 1 S T 1 S T41 S T58 S T227£101AvilaBeachEdnaGardenFarmsLosOsosMorroBayPismoBeachPort SanLuisSan LuisObispoSantaMargaritaThylePointBuchonPointSan LuisDCPP-120°37'-120°37'-120°44'-120°44'-120°51'-120°51'35°25'35°25'35°18'35°18'35°11'35°11'Irish Hills Study Area and 2011Onshore Seismic Reflection Data
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_PacificOceanDCPPSantaBarbaraArroyoGrande1-1Figure extent
+/-0 2 4mi.0 4 8kmEXPLANATION2011 ONSIPSeismic Reflection Survey2011 vibroseis line2011 AWD line and 2011 vibroseis lineFigurePacific Gas and Electric Company2011 nodal receivers, no shotpoints2011 nodal receiver array!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!Map projection and scale:1:175,000NAD 1983 l UTM Zone 10N,InterstatesHighwaysMajor roads2011 AWD line File path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_2-01.ai; Date: 06/04/2014; User: Jereme Chandler, LCI; Rev.1Pacific Gas and Electric Company FigureTectonic Setting 2-12011 ONSIPzoneBank fault Q u e e n i e C L S M A P H VEsteroBayPoint Argue ll o DCPP Point Conception C a m b r i a F a u l t W i l m a r A v e n u e f a u l t L i o n s H e a d f a u l t f a u l t z o n e S W b o u n d a r y R i n c o n a d a F a u l t S a n A n d r e a s f a u l t z o n e N a c i m i e n t o f a u l t z o n e S a n S i m e o n f a u l t z o n e Piedras Blancas anticlinorium H o s g r i f a u l t z o n e P u r i s i m a s t r u c t u r e L o m p o c s t r u c t u r e S a n t a Y n e z R i v e r C a s m a l i a f a u l t z o n e L o s O s o s f a u l t z o n e f a u l t z o n e O c e a n o f a u l t O c e a n i c - W e s t H u a s n a f a u l t z o n e S O U T H E R N C O A S T R A N G E S S A N T A L U C I A R A N G E S A N R A F A E L R A N G E LOS OSOS DOMAIN OFFSHORE SANTA MARIA BASIN WESTERN TRANSVERSE RANGES EF 0 20 km 120° 30' 120° 121° 30' 121° 120° 30' 120°34° 30' 35° 00' 35°30' 35° 30' 36°00' 36° 00'EXPLANATION Uplifted structural blocks within the Los Osos domain, outlined by thick gray line Structural blocks within the Los Osos domain A = Casmalia C = Cambria H = Solomon Hills
L = Los Osos M = Santa Maria Valley P = Purisima
S = San Luis/Pismo
V = Vandenberg/Lompoc Sources: PG&E (1988, 2011); regional tectonic sketch map from (Hanson et al., 2004).
Boundary outlining Los Osos domain EF = Edna Fault Figure extentAREA OF INSET MAP File path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_2-02.mxd; Date: 06/26/2014; User: Alex Remar, LCI; Rev.1
^_!A!A!A!A!A!ALOSOSOSFAULTZONEEdna AZONESANMIGUELITOFAULTSANLUISBAYFAULTZONESHORELINEFAULTZONEPismo SynclineEdna BEdna Fault ZoneKjfoTmodTmodTmoTmoTmmTmpmTmoQlsQlsTmmOlsonHillQswQs KsTmoTmmQswTpps Ks KsTppsTmoTmpmKJfmQswTmmQm s sTmpmTmrQoaQalTmpmKJfmKJfmvKJfgQalKJfmKJfmKJfgTmpmQcQeKJfmKJfmvQoaKJfmv sQsQeQalMaino-Gonzales 1Pecho 1Spooner 1Honolulu-Tidewater 1Montadoro 1Townsend-Gunter 1PointSan LuisLos OsosPort SanLuisDCPPGreenPeakLionRockPointBuchonOatsPeak-120°45'-120°45'-120°50'-120°50'-120°55'-120°55'35°15'35°15'35°10'35°10'Map projection and scale: WGS 84 / UTM Zone 10N,1:70,000µEXPLANATION
^_DCPPCambriaSan Luis ObispoFigure extentGeologic Map of the Irish Hills2-22011 ONSIP
+/-0 1 2mi.0 1 2kmNotes: See Plate 1 for full list of geologic units.Offshore geology from PG&E (2011).Wells!APacificOceanPacific Gas and Electric CompanyFigure File path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_2-03.ai; Date: 06/04/2014; User: Alex Remar, LCI; Rev.1Pacific Gas and Electric Company Figure Stratigraphy of the Irish Hills 2-32011 ONSIP Unit Thickness Unit Age Description Surficial Deposits
~0.5 Ma to present Pismo Formation (upper)Squire Member Belleview Member Gragg Member Pismo Formation (lower)unconformity 3.3 to 3.0 Ma unconformity unconformity Miguelito Member Pliocene Pleist.Monterey Formation Quat.Edna Member unconformity progressive unconformityTertiary Miocene Oligocene unconformity unconformity/intrusive/faulted unconformity Cretaceous Jurassic-Cretaceous faulted Obispo Formation Rincon FormationVaqueros Formation Sandstone Franciscan Complex (also serpentine)10 to 80 ft550 ft650 ft550 ft2,250 ft1,450 ft> 2,000 ft1,350 ft (1,000 to 2,000 ft on map)500 ft> 2,500 ft> 2,000 ft(?)
10.4 to 9.0 Ma~4.2 Ma11.4 to 10.5 Ma 15.5 to 15.3 Ma Belleview Member of the Pismo Formation (Tppb): Interbedded buff to
light gray claystone and fine-grained sandstone, weakly to moderately well
lithified, fossiliferous horizons, diatomaceous horizons, claystone fractures spheroidally. Basal contact with Gragg Member is generally conformable.
Squire Member of the Pismo Formation (Tpps):
Unstratified white fine-to medium-grained silty sandstone, poorly lithified, fossiliferous horizons, rare pholad-bored cobbles where Squire Member unconformably overlies
basement rock. Basal contact with Belleview Member is generally
conformable.
Gragg Member of the Pismo Formation (Tppg):
Unstratified white to buff fine- to medium-grained sandstone, poorly to moderately well-lithified, rare diatomaceous siltstone, pebble conglomerate, and bituminous
sandstone. Basal contact with lower members of the Pismo Formation is
unconformable.
Edna Member of the Pismo Formation (Tmpe): Thickly bedded to unstratified gray to brown fine- to coarse-grained sandstone, moderately
well-lithified, common bituminous horizons, basal chert pebble conglomer-
ate (Tmpec) and tuffaceous sandstone horizons. Grades laterally into the
Miguelito Member to the west and south.
Miguelito Member of the Pismo Formation (Tmpm): Thinly bedded brown siltstone and claystone, moderately well-lithified, rare to common
intervals of siliceous and dolomitic siltstone, opaline and porcelaneous
shale, and bituminous sandy siltstone. Basal contact with Monterey
Formation at Point Buchon is relatively gradual but is described by Hall (1973a, 1973b) as unconformable elsewhere in San Luis Obispo County.
Monterey Formation (Tmm):
Clastic sub-unit (Tmmb) is thinly bedded dolomitic siltstone and shale (lesser chert), siliceous sub-unit (Tmmc) is thinly bedded siliceous shale and chert (lesser dolomitic siltstone and
claystone), diatomaceous sub-unit (Tmmd) is diatomite (lesser shale and chert), tuffaceous subunit (Tmmt) is tuffaceous siltstone. Generally white, gray, and brown and weathers to chalky white, well-lithified with a conchoi-
dal fracture habit, fractured and sheared. Basal contact along coast grades from interbedded fine-grained diatomaceous and tuffaceous sandstone of Tmof into interbedded chert and sandstone/siltstone of Tmmb.
Obispo Formation (Tmo):
Resistant sub-unit (Tmor) is crudely bedded to unstratified, orange-brown to gray fine-grained zeolitized tuff, very
well-lithified, chaotic, unstratified intervals with basal scour and rare
intervals of black silty sandstone. Fine-grained subunit (Tmof) is well-
bedded light brown to gray sandstone and silty sandstone, coarsening
gradually up-section, including abundant invervals of dolomitic sandstone and common intervals of diatomaceous and tuffaceous sandstones.
Diabase sub-unit (Tmod) is brown aphanitic to phaneritic intrusive dikes and sills. Tuffaceous sub-unit (Tmot) is grouped with Tmor sub-unit along the coastline at DCPP but is mapped by Hall (1973a, 1973b) elsewhere in San Luis Obispo County. Basal contact with Rincon Formation is not
exposed along coastline but is mapped as conformable in the Irish Hills by
Hall (1973a). Contact with basement rock along coastline may be
depositional, intrusive, or faulted.
Rincon Formation (Tmr): Thinly bedded dark brown siltstone and silty
claystone with interbeds of dolomitic sandstone. Not exposed along
coastline but mapped as conformable by Hall (1973b).100 ftVaqueros Formation (Tov): Tan to gray conglomerate and sandstone.
Not exposed along coastline but mapped in the Irish Hills by Hall (1973b).
Cretaceous Sandstone (Ks): Well-bedded brown fine- to coarse-
grained sandstone, moderately to very well-lithified, generally quartz grains with minor feldspar and lithic grains. Also includes yellowish brown
to black fissile shale, and dark brown fine- to medium-grained, unstrati-fied vesicular basalt and diabase. Abuts Franciscan Complex rock along
faulted contacts.
Franciscan Complex (KJf):
Chaotic, unstratified assemblage of varying lithologies, including fine-grained metavolcanic rocks (with strong
magnetic resistivity values), sheared claystone (melange matrix),
glaucophane schist, and chert. Serpentine is included in Franciscan Complex. Regionally, graywacke sandstone is a prominent component of
the Franciscan Complex but is not common within the mapped area
described in this report.
Surficial deposits:
Stream alluvium, marine terraces, fluvial terraces, landslides, beach sand, and sand waves, unlithified.
Source: Figure modified from Hall (1973b)Undifferentiated Mesozoic BasementUndifferentiated Obispo, Rincon,and Vaqueros Formations Careaga Formation equivalent to upper Pismo Formation (Hall, 1973b)
KjfTmoTmm Seismic Interpretation UnitsTpc EO-CENELATE EPOCH TIDEWATER SW SW NE NE MONTANA DE ORO IRISH HILLS STRATIGRAPHY (This Study) 25 26 27 28 29 30 31 32 33 34 35LATE OLIGOCENEEARLY Pleist.PlioceneLATE 5 6 7 8 9 1011 12 4 3 2 1 L MIOCENE MIDDLEEARLY 23 24 TIME (Ma)15 16 17 18 19 20 21 22 E 14 13 BENTHIC FORAMINIFERAL ZONE (bfz)
Refugian Zemorrian Vaqueros Vaqueros?
(not exposed)
Rincon?(not exposed)
Obispo Morro-Islay?Obispo Monterey Monterey Paso Robles?Careaga?U. Pismo Qmt Qmt L. Pismo Miguelito L. Pismo Miguelito Rincon Rincon Vaqueros Saucesian Relizian Luisian Mohnian Delmontian RepettianVenturian Wheelerian Hallian E M Edna EdnaModi~ed from McDougall (2008)
TERTIARY STRATIGRAPHY OF THE PISMO SYNCLINE IN THE IRISH HILLS COASTAL ONLAP 0 50 100 150 200 250 meters minor major medium sequence boundariesFile path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_04.ai; Date: 02/19/2014; User: S. Thompson, LCI; Rev.1 Figure Pacific Gas and Electric CompanyTertiary Stratigraphy of the Pismo Syncline in the Irish Hills 2-42011 ONSIPVertical lines represent missing stratigraphic section.Note: Epoch, benthic foraminiferal zones, and coastalonlap data are from McDougall (2008). Irish Hills stratigraphy modi~ed from Hall (1973b). See Section 2.0 for further discussion and additional references.
File path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_2-05.mxd; Date: 06/10/2014; User: Alex Remar, LCI; Rev.2 mmmmmmmmmmmmmmmmmmmmmmmmmm^
_HOSGRI FAULT ZONELOS OSOS FAULT ZONESAN LUIS BAY FAULTSAN MIGUELITO FAULTEDNA FAULT ZONESHORELINEFAULTZONEArroyoGrandeLos OsosMorroBayPismo BeachPort San LuisSan Luis ObispoGreen PeakLion RockPoint BuchonOats PeakQuarryCoveDCPP-120°40'-120°40'-120°50'-120°50'-121°0'-121°0'35°20'35°20'35°10'35°10'Map projection and scale: WGS 84 / UTM Zone 10N,1:120,000µEXPLANATION
^
_DCPPFigure extentEarthquake Epicenters andComplete Gravity Bouguer Anomaly2-52011 ONSIP
+/-0 2 4mi.0 2 4kmEarthquake DataMagnitude2.0 - 2.93.0 - 3.50.0 - 0.9 1.0 - 1.9Depth (Km)Note:Quaternary fault traces compiled and modified from Lettisand Hall (1994), Lettis et al. (2004), AMEC (2011), PG&E (2013),
and this study.Sources: Relocated earthquake data from Hardebeck (2014);Gravity data from Langenheim et al. (2014).PacificOceanFault, solid where well located, dashed where approximately located, dotted where inferred, queried where existence uncertain.
?Complete Bouguer Anomaly (mGal)Pacific Gas and Electric CompanyFigure201510 5 0-5-10-15-20 30-350.0 - 1.92.0 - 3.94.0 - 5.96.0 - 7.910.0 - 11.98.0 - 9.914.0 +12.0 - 13.9 Note: Marine magnetic data were filtered to effectively place those data at the same height as the aeromagnetic data (~305 m) (Langenheim et al., 2009).File path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_2-06.ai; Date: 06/10/2014; User: Alex Remar, LCI; Rev.1 Figure Pacific Gas and Electric Company Merged Aeromagnetic and Marine Magnetic Data 2-62011 ONSIP DCPP File path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_3-01.ai; Date: 06/10/2014; User: Jereme Chandler, LCI; Rev.1Pacific Gas and Electric Company Figure Organization Chart for the Onshore Seismic Reflection Interpretation Project 3-12011 ONSIP Stuart Nishenko (PG&E)
Seismic Interpretation Team Support Staff 2011 Onshore Seismic Interpretation Project Manager Jeffrey Unruh (LCI)
Robert Givler (LCI)
Dan O'Connell (Fugro)
James Turner (Fugro)
Josh Goodman (Fugro) 2011 Onshore Seismic Interpretation Independent Technical Reviewer (ITR)
Robert Yeats (ECI)(LCI)Marcia McLaren (PG&E)
Project Technical Advisor Support Staff (Fugro)Technical Coordinator Quality Assurance Manager Megan Stanton (PG&E)
Quality Assurance Records Coordinator Michael Angell (Fugro)
Database Manager Serkan Bozkurt (LCI)
File path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-01.mxd; Date: 06/26/2014; User: Alex Remar, LCI; Rev.1
!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!J J J J J J J J J J J J^_!A!A!A!A!A!ALOSOSOSFAULTZONEEdna AZONESANMIGUELITOFAULTSANLUISBAYFAULTZONESHORELINEFAULTZONEEdna B141-142 S141-142 N204 W103 - 104112 - 140 CC'BB'BFF'E'E DD'AAA'0400080001200016000200002400028000 04000800012000 04000800012000 0400080001200016000200002400028000320003600080002000040001200016000204Maino-Gonzales 1Pecho 1Spooner 1Honolulu-Tidewater 1Montadoro 1Townsend-Gunter 1DCPPQswTmoQsKJfo KsKJfQmTmoTmmKJfmQswTppsTppb KsKJfmTppgTmoKJfQm KsTppsQalTmoTmodQmQlsTmoQlsQswTmmKJfmvTmo s sTmpmTmrQmQlsQalTmpmQlsKJfmQafKJfmKJfgTmpeKJfmvQalQalQeKJfmvKJfgTmpmQcQoaQswTomQlsQeKJfmKJfmvQoaKJfmv sQsQeQal-120°45'-120°45'-120°50'-120°50'-120°55'-120°55'35°15'35°15'35°10'35°10'µEXPLANATION
^_DCPPCambriaSan Luis ObispoFigure extentKey Seismic Lines Imagingthe Pismo Syncline5-12011 ONSIP
+/-0 1 2mi.0 1 2kmNotes: See Plate 1 for full list of geologic units. Offshoregeology from PG&E (2011).Geologic cross section J JHorizontal distance along seismic line,2,000 ft. IncrementWells with elevation of top of Monterey FormationVibroseis seismic reflection lineAWD seismic reflection linePacificOcean!A!Pacific Gas and Electric CompanyFigureMap projection and scale: WGS 84 / UTM Zone 10N,1:70,000 DCPPFile path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-02_Line_103_104_AWD_LCI.mxd; Date: 06/10/2014; User: Jereme Chandler, LCI; Rev.1Notes:- Seismic line103-104_AWD_FBM_psdm_ 1_mix_depth_tvfagc.- Geology along topographic profile from Plate 1; see Plate 1 and Figure 5-1 for explanation of map units.- See Plate 2 for full-scale interpreted seismic line with geologic strip map.
- Horizontal offsets are shown along a topographic profile above the seismic line.5-2AWD Line 103-104:(a) Uninterpreted and (b) Interpreted2011 ONSIPPacific Gas and Electric CompanyFigureSeismic line in redTop of Rincon FormationTmrEXPLANATIONFault: solid where well located,dashed where approximately locatedTop of Monterey FormationTop of Obispo FormationTop of Mesozoic basementTmmTmoKJfHorizontal distance alongseismic line, 2,000 ft increment(b)Interpreted(a)UninterpretedArrows marking offset or truncated reflectors DCPPFile path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-03_Line_103_104_AWD_Fugro.mxd; Date: 06/10/2014; User: Jereme Chandler, LCI; Rev.1Notes:- Seismic line QA_bpfagc_103_104_AWD_FBM_psdm _1_mix_depth_notvfagc_ieee.- Geology along topographic profile from Plate 1; see Plate 1 and Figure 5-1 for explanation of map units.- Horizontal offsets are shown along a topographic profile above the seismic line.5-3Alternative Interpretation ofAWD Line 103-104:(a) Uninterpreted and (b) Interpreted2011 ONSIPPacific Gas and Electric CompanyFigureTop of Edna FormationTop of Vaqueros FormationSeismic line in redTop of Rincon FormationTmrEXPLANATIONFault: solid where well located,dashed where approximately locatedTop of Monterey FormationTop of Obispo FormationTop of Mesozoic BasementTmmTmoKJfHorizontal distance alongseismic line, 2,000 ft incrementTovTmpe(b)Interpreted(a)Uninterpreted DCPPFile path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-04_Line_204_AWD_LCI.mxd; Date: 06/10/2014; User: Jereme Chandler, LCI; Rev.15-4AWD Line 204:(a) Uninterpreted and (b) Interpreted2011 ONSIPNotes:- Seismic line 204_AWD_FBM_psdm_1_mix_depth_tvfagc.- Geology along topographic profile from Plate 1, see Plate 1 and Figure 5-1 for explanation of map units.
- See Plate 3 for large-scale interpreted seismic line with geologic strip map.- Horizontal offsets are shown along a topographic profile above the seismic line.Pacific Gas and Electric CompanyFigureSeismic line in redEXPLANATIONFault: solid where well located,dashed where approximately locatedTop of Monterey FormationTop of Obispo FormationTop of Rincon FormationTop of Mesozoic BasementTmmTmoKJfTmrHorizontal distance alongseismic line, 2,000 ft increment(a)Uninterpreted(b)InterpretedArrows marking offsetor truncated reflectors DCPPFile path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-05_Line_204_Vibe_West.mxd; Date: 06/10/2014; User: Jereme Chandler, LCI; Rev.15-5Vibroseis Line 204 West:(a) Uninterpreted and (b) Interpreted2011 ONSIPEXPLANATIONNotes:- Seismic line trimmed_204_west_2D_beam_50K_vibeonly_ poly_sl_stackagc_IEEE_uninterpMay13.- Geology along topographic profile from Plate 1; see Plate 1 and Figure 5-1 for explanation of map units.- See Plate 4 for large-scale interpreted seismic line with geologic strip map.- Horizontal offsets are shown along a topographic profile above the seismic line.Pacific Gas and Electric CompanyFigureSeismic line in redFault: solid where well located,dashed where approximately locatedTop of Monterey FormationTop of Obispo FormationTop of Rincon FormationTop of Mesozoic Basement FormationTmmTmoKJfTmrHorizontal distance alongseismic line, 2,000 ft increment(a)Uninterpreted(b)InterpretedArrows marking offsetor truncated reflectors DCPPFile path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-06_Line_204_AWD_Fugro.mxd; Date: 06/10/2014; User: Jereme Chandler, LCI; Rev.15-6Alternative Interpretation of AWD Line 204:(a) Uninterpreted and (b) Interpreted2011 ONSIPNotes:- Seismic line QA_bpfagc_204_AWD_FBM_psdm_1_mix_depth_notvfagc_ieee.- Geology along topographic profile from Plate 1, see Plate 1 and Figure 5-1 for explanation of map units.
- Horizontal offsets are shown along a topographic profile above the seismic line.Pacific Gas and Electric CompanyFigureSeismic line in redEXPLANATIONFault: solid where well located,dashed where approximately locatedTop of Monterey FormationTop of Obispo FormationTop of Rincon FormationTop of Mesozoic BasementTmmTmoKJfTmrHorizontal distance alongseismic line, 2,000 ft incrementTop of Pismo Formation,Edna MemberTmpe(a)Uninterpreted(b)InterpretedArrows marking offsetor truncated reflectors DCPPFile path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-07_Line_112_140_AWD_LCI.mxd; Date: 06/10/2014; User: Jereme Chandler, LCI; Rev.15-7AWD Line 112-140:(a) Uninterpreted and (b) Interpreted2011 ONSIPNotes:- Seismic line QA_bpfagc_dwf 112-140 AWD fbm psdm 1 mix depth notvfagc ieee.- Geology along topographic profile from Plate 1; see Plate 1 and Figure 5-1 for explanation of map units.
- See Plate 3 for large-scale interpreted seismic line with geologic strip map.- Horizontal offsets are shown along a topographic profile above the seismic line.Pacific Gas and Electric CompanyFigureSeismic line in redEXPLANATIONFault: solid where well located,dashed where approximately locatedTop of Monterey FormationTop of Obispo FormationTop of Mesozoic BasementTmmTmoKJfHorizontal distance alongseismic line, 2,000 ft increment(a)Uninterpreted(b)InterpretedArrows marking offset or truncated reflectors DCPPFile path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-08_Line_112_140_AWD_Fugro.mxd; Date: 06/10/2014; User: Jereme Chandler, LCI; Rev.15-8Alternative Interpretation ofAWD Line 112-140:(a) Uninterpreted and (b) Interpreted2011 ONSIPNotes:- Seismic line QA_bpfagc_dwf_112-140_AWD_fbm_psdm_1_mix_depth_notvfagc_ieee.- Geology along topographic profile from Plate 1; see Plate 1 and Figure 5-1 for explanation of map units.
- Horizontal offsets are shown along a topographic profile above the seismic line.Pacific Gas and Electric CompanyFigureSeismic line in redEXPLANATIONFault: solid where well located,dashed where approximately locatedTop of Monterey FormationTop of Obispo FormationTop of Mesozoic BasementTmmTmoKJfHorizontal distance alongseismic line, 2,000 ft incrementTop of Rincon FormationTmr(a)Uninterpreted(b)InterpretedArrows marking offsetor truncated reflectors DCPPFile path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-09_Line_141_142_South.mxd; Date: 06/10/2014; User: Jereme Chandler, LCI; Rev.15-9Vibroseis Line 141-142 South:(a) Uninterpreted and (b) Interpreted2011 ONSIPPacific Gas and Electric CompanyFigureSeismic line in redNotes:- Seismic line 2011 3D Arb straight south 141-142 IEEE.- Geology along topographic profile from Plate 1; see Plate 1 and Figure 5-1 for explanation of map units.
- See Plate 6 for large-scale interpreted seismic line with geologic strip map.- Horizontal offsets are shown along a topographic profile above the seismic line.EXPLANATIONFault: solid where well located,dashed where approximately locatedTop of Monterey FormationTop of Obispo FormationTop of Mesozoic BasementTmmTmoKJfHorizontal distance alongseismic line, 2,000 ft increment(a)Uninterpreted(b)InterpretedArrows marking offsetor truncated reflectors File path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-10_Line_141_142_North.mxd; Date: 06/10/2014; User: Jereme Chandler, LCI; Rev.1EXPLANATIONNotes:- Seismic line 2011 3D Arb straight north 141-142 IEEE.- Geology along topographic profile from Plate 1; see Plate 1 and Figure 5-1 for explanation of map units.
- See Plate 6 for large-scale interpreted seismic line with geologic strip map.- Horizontal offsets are shown along a topographic profile above the seismic line.5-10Vibroseis Line 141-142 North:(a) Uninterpreted and (b) Interpreted2011 ONSIPPacific Gas and Electric CompanyFigureFault: solid where well located,dashed where approximately locatedTop of Monterey FormationTop of Obispo FormationTop of Mesozoic BasementTmmTmoKJfHorizontal distance alongseismic line, 2,000 ft increment(a)Uninterpreted(b)InterpretedArrows marking offsetor truncated reflectorsDCPPSeismic line in red DCPPFile path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-11_Line_141_142_North_South_Combined.mxd; Date: 06/10/2014; User: Jereme Chandler, LCI; Rev.1Notes:- Seismic line 2011 3D Arb straight north 141-142 IEEE and 2011 3D Arb straight south 141-142 IEEE.- Geology along topographic profile from Plate 1; see Plate 1 and Figure 5-1 for explanation of map units.- See Plate 6 for large-scale interpreted seismic line with geologic strip map.- Horizontal offsets are shown along a topographic profile above the seismic line.5-11Vibroseis Line 141-142, North and South:Segments Joined2011 ONSIPPacific Gas and Electric CompanyFigureSeismic line in redEXPLANATIONFault: solid where well located,dashed where approximately locatedTop of Monterey FormationTop of Obispo FormationTop of Mesozoic BasementTmmTmoKJfHorizontal distance alongseismic line, 2,000 ft incrementArrows marking offsetor truncated reflectors File path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-12.mxd; Date: 06/26/2014; User: Alex Remar, LCI; Rev.1
@@@@@@@@@@@@@@@@@@@lllllllll@@@llllllll@@@@@@@@@@@@@lllllllllll@@@@@@@@@@@@@@llllll@@@@@@@@@@@@@lll@@@llllllllllllllllll^_!A!A!A!A!A!A!A!A!A!A!A!A!A!A!A°º°°°ZONESANLUISBAYFAULTZONEFAULTZONE 0112-140141-142 N112-140141-142 S103-104141-142 N204207Los Osos ValleyIrish Hills
????????ContoursNotConstrainedFranciscan Complex ExposedFranciscan ComplexExposed?CretaceousSandstone (Ks)ExposedKsOld SeeCanyon 1Maino-Gonzales 1-1,251 ft.Spooner 1-1,218 ft.Honolulu-Tidewater 1below -9,157 ft.Montadoro 1below -5,765 ft.Townsend-Gunter 1-2,379 ft.Townsend-Peterson 1CCWPechoS&T newLOCSD -SB deepCCW -SB#1LOCSD -Ferrell #2LOCSD -10th newLOCSD -PalisadesUSGS -PalisadesEdna CFault 2Fault 1Fault 3Fault 2Edna BEdna AFault 4Edna CFault 4Fault 3Edna CEdna AEdna BDCPP-1500500500 0-500-1000-1500-3500-4000-6000-8000-90001000-1500-2000-2500-2000-4000-6000-3000-2000500 0-500-1000-4000-50001000-3000500-3000500 0-1000-2000-30001000-1000-2500 0-120°45'-120°45'-120°50'-120°50'35°15'35°15'Map projection and scale: WGS 84 / UTM Zone 10N,1:52,000µ^_DCPP San Luis ObispoFigure extentStructure Contours:Elevation of Top of Mesozoic Basement5-122011 ONSIP
+/-0 1 2mi.0 1 2kmNotes:- Maximum contour interval = 1,000 ft, additional contours are shown in some locations.- See Figure 2-2 and Plate 1 for an explanation of geologic map units.EXPLANATIONPlunging syncline
ºSeismic/CDP linesElevation of Top of Mesozoic basement (ft),queried where uncertain
?Wells with picks for elevation of top of basement
!APacificOceanPacificOceanApproximate limit of Tertiary exposureFault: solid where well located, dashed whereapproximately located, short dashed where offset is less than contour interval, queried where uncertain
?Plunging anticline
°Pacific Gas and Electric CompanyFigureMesozoic basement below depth of imaging File path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-13.mxd; Date: 06/10/2014; User: Alex Remar, LCI; Rev.1
@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@llllllllllllll@@@llllll@@@@@@@llllllllll#############################################################################################llllllllllll@@@@@@@@@@@lllllllllllºº^
_!A!A!A!A!A!A!A!A!A!A!A!A!A!A!AZONESANLUISBAYFAULTZONE 0 0500-3000141-142 N204141-142 S112-140103-104207Approximate Limit of Tertiary Exposure Appr o x i m a t eLi m i t o f T e r t i a r y E x p o s u r eLos Osos ValleyIrish HillsMesozoicBedrock ExposedMesozoicBedrock Exposed
?????????????????Montadoro 1-3,419 ft.Top of ObispoFormation ContactOld SeeCanyon 1Maino-Gonzales 1 (Tmo not present)Spooner 1(Tmo not present)Honolulu-Tidewater 1-2,732 ft.Townsend-Gunter 1-534 ft.Townsend-Peterson 1CCW PechoS&T newLOCSD -
SB deepCCW -
SB#1LOCSD -
Ferrell #2LOCSD -10th newLOCSD -
PalisadesUSGS -Palisades-4000-3000-2500-3000-1500-2000-3000-1000500 0500 0-500-1000-1500-1500-2000-25001000-1500-3500 0-500-2000-2500-3000-4500-1000500 0-2000-2500-4000500-2000-3000-4000-4500-5000-5000-5500-500-10001000500-4500Fault 1 E d n a A s p l a yFault 0Fault 1Fault 2Fault 3Northern Extent of TmoEdna CFault 4Edna AEdna AFault 2Fault 3Edna CEdna BDCPP-120°45'-120°45'-120°50'-120°50'35°15'35°15'Map projection and scale: WGS 84 / UTM Zone 10N,1:52,000
µ^
_DCPPSan Luis ObispoFigure extentStructure Contours:Elevation of Top of Obispo Formation5-132011 ONSIP
+/-0 1 2mi.0 1 2kmNote: Contour interval = 500 ft.EXPLANATIONWells with elevation of top of Obispo FormationSynclineºFault: solid where well located, dashed whereapproximately located, short dashed where offset is less than contour interval, queried where uncertain
?Elevation of top of Obispo Formation (ft), dashed where approximately located, queried where uncertain
?!APacificOceanPacificOceanTop of Obispo contact from geologic mapping (Plate 1)Approximate limit of Tertiary exposurePacific Gas and Electric CompanyFigureSeismic/CDP lines File path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-14.mxd; Date: 06/10/2014; User: Alex Remar, LCI; Rev.1 llllllll@@@@@@@@@@@@@@lll@@@@@llllll@lllllllllll@@+++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++@@@@@@@@llllllllll@@@@@@@@@@@lll@@@llllll@@@@@°º°°ºº^
_!A!A!A!A!A!A!A!A!A!A!A!A!A!A!AZONESANLUISBAYFAULTFAULTZONE 0Tips OutTips Out-800141-142 N204141-142 S112-140103-104207 A p p r o x i m a t e Limit o f T e r t i a r yEx p o s u r eApproximate Limit of Tertiary ExposureLos Osos ValleyIrish HillsMesozoicBedrock ExposedMesozoicBedrock ExposedNorthern Extent of Tmm
????Top of MontereyFormation ContactOld SeeCanyon 1Maino-Gonzales 1(Tmm not present)Spooner 1(Tmm not present)Honolulu-Tidewater+594 ft.Montadoro 1-1,319 ft.Townsend-Gunter 1-232 ft.Townsend-Peterson 1CCW PechoS&T newLOCSD -
SB deepCCW -
SB#1LOCSD -
Ferrell #2LOCSD -10th newLOCSD -
PalisadesUSGS -Palisades800-1600400-1800 0-400400-1200-400-400400-800 0-400-400-1600-1200-400800400400-1600-2000-2000-2400-400-1200-2400400 0-800400 0800 0 0Edna AEdna CEdna CEdna AFault 1Fault 2Fault 3Edna CEdna BDCPP-120°45'-120°45'-120°50'-120°50'35°15'35°15'Map projection and scale: WGS 84 / UTM Zone 10N,1:52,000
µ^
_DCPPSan Luis ObispoFigure extentStructure Contours:Elevation of Top of Monterey Formation5-142011 ONSIP
+/-0 1 2mi.0 1 2kmNote: Contour interval = 400 ft.EXPLANATIONFault: solid where well located, dashed whereapproximately located, short dashed where offset is less than contour interval, queried where uncertain
?Elevation of top of Monterey Formation (ft), dashed where approximately located, queried where uncertain
?PacificOceanPacificOceanTop of Monterey contact from geologic mapping (Plate 1)Approximate limit of Tertiary exposureWells with elevation of top of Monterey Formation
!APacific Gas and Electric CompanyFigurePlunging anticline
°Plunging syncline
ºSeismic/CDP lines File path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-15.mxd; Date: 06/27/2014; User: Alex Remar, LCI; Rev.1
!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!A!A!A!A!A!A!A!A!ACleath &Associates (2003)Los Osos ValleyMorroBay103-104 0 s20006000 0400080001200016000200002400026000280003000032000200060001000014000160001800020000 0200040006000Maino-Gonzales 1Spooner 1CCWPechoLOCSD -SB deepCCW -SB#1LOCSD -Ferrell #2LOCSD -10th newLOCSD -PalisadesUSGS -Palisades30S/10E-13H30S/10E-13M1(GS-1)30S/10E-14B130S/11E-17J1(GS-3)30S/11E-18M130S/11E-19H2(GS-6)30S/11E-20Aa30S/11E-20Ea30S/11E-20G02(GS-5)30S/11E-20J30S/11E-20L30S/11E-20M130S/11E-21D1530S/11E-21D430S/10E-24A2(GS-4)30S/11E-7Q330S/11E-8M230S/11E-22J129S/11E-32K229S/11E-32M130S/10E-12J1(MBO-5)4000800012000207117118121105180002000022000240002600028000300003400038000 47 36 14 38 76 43 48 47 24 80 80 30 22 32 25 50 40 20 25 20 15 20 45 70 15 65 47 32 15 25 25 35 50 55 45 25 30 50 20 29 30 70 60 40 35 35 50 40 35 67 45 50 70 85 60 50 25 20 80 48 60 30 65 45 40 47 45 55 47 72 52 35 65 36 26TovKJfmKJfgTmrQlsTmpeQmKJfmvKJfgKJfgKJfmQeQlsTmpmKJfmvQalQal schKJfgQalTmpmQcQafQeQoaKJfmvQal sQsTomKJfmTomQoaKJfmQlsQlsQeQalQalQes-120°50'-120°50'35°20'35°20'Map projection and scale: WGS 84 / UTM Zone 10N,1:30,000µEXPLANATION
^
_DCPPSan Luis ObispoFigure extentAWD and Vibroseis Seismic LinesWithin Los Osos Valley5-152011 ONSIP
+/-00.5 1mi.00.5 1kmNote: See Plate 1 for full list of geologic units and symbols.Vibroseis seismic reflection line Cleath & Associates (2003, 2005) boreholesPacific Gas and Electric CompanyFigureHorizontal distance along seismic line,2,000 ft. incrementAWD seismic reflection line PacificOceanWells and boreholes compiled by GMP(PG&E, 2014)
!A!
DCPPFile path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-16_Line_207.mxd; Date: 06/10/2014; User: Jereme Chandler, LCI; Rev.1EXPLANATIONFault: solid where well located,dashed where approximately locatedNotes:- Seismic line 207 awd fbm psdm 1 mix depth tvfagc.- Geology along topographic profile from Plate 1; see Plate 1 and Figures 2-2 and 5-1 for explanation of map units.
- Horizontal offsets are shown along a topographic profile above the seismic line.5-16AWD Line 207:(a) Uninterpreted and (b) Interpreted2011 ONSIPPacific Gas and Electric CompanyFigureSeismic line in redTop of Mesozoic BasementHorizontal distance alongseismic line, 2,000 ft increment(a)Uninterpreted(b)InterpretedArrows marking offsetor truncated reflectors DCPPFile path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-17_Line_105.mxd; Date: 06/10/2014; User: Jereme Chandler, LCI; Rev.15-17Vibroseis Line 105:(a) Uninterpreted and (b) Interpreted2011 ONSIPEXPLANATIONFault: solid where well located,dashed where approximately locatedNotes:- Seismic line trimmed_105_2D_beam_50k_vibeonly_poly_sl_stackagc_IEEE.- Geology along topographic profile from Plate 1; see Plate 1 and Figure 6-1 for explanation of map units.
- Horizontal offsets are shown along a topographic profile above the seismic line.Pacific Gas and Electric CompanyFigureSeismic line in redTop of Careaga FormationTpcTop of Mesozoic BasementKJfHorizontal distance alongseismic line, 2,000 ft increment(a)Uninterpreted(b)Interpreted DCPPFile path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-18_Line_117.mxd; Date: 06/10/2014; User: Jereme Chandler, LCI; Rev.15-18AWD Line 117:(a) Uninterpreted and (b) Interpreted2011 ONSIPEXPLANATIONFault: solid where well located,dashed where approximately locatedNotes:- Seismic line 117 AWD FMB tvfagc.- Geology along topographic profile from Plate 1; see Plate 1 and Figure 6-1 for explanation of map units.
- Horizontal offsets are shown along a topographic profile above the seismic line.Pacific Gas and Electric CompanyFigureSeismic line in redTop of Mesozoic BasementTop of Careaga FormationTop of Pismo Formation, undifferentiatedHorizontal distance alongseismic line, 2,000 ft incrementTpcTmpKJf(a)Uninterpreted(b)InterpretedArrows marking offset or truncated reflectors DCPPFile path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-19_Line_117_Alternative.mxd; Date: 06/10/2014; User: Jereme Chandler, LCI; Rev.15-19Alternative Faulting Interpretation ofAWD Line 117: (a) Uninterpreted and(b) Interpreted2011 ONSIPPacific Gas and Electric CompanyFigureSeismic line in redEXPLANATIONFault: solid where well located,dashed where approximately locatedTop of Mesozoic BasementTop of Careaga FormationTop of Pismo Formation, undifferentiatedHorizontal distance alongseismic line, 2,000 ft incrementTpcTmpKJfNotes:- Seismic line 117 AWD FMB tvfagc.- Geology along topographic profile from Plate 1; see Plate 1 and Figure 6-1 for explanation of map units.
- Horizontal offsets are shown along a topographic profile above the seismic line.(a)Uninterpreted(b)InterpretedArrows marking offset or truncated reflectors DCPPFile path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-20_Line_118.mxd; Date: 06/10/2014; User: Jereme Chandler, LCI; Rev.15-20AWD Line 118:(a) Uninterpreted and (b) Interpreted2011 ONSIPEXPLANATIONFault: solid where well located,dashed where approximately locatedNotes:- Seismic line 118 AWD FBM tvfagc.- Geology along topographic profile from Plate 1; see Plate 1 and Figure 6-1 for explanation of map units.
- Horizontal offsets are shown along a topographic profile above the seismic line.Pacific Gas and Electric CompanyFigureSeismic line in redTop of Mesozoic basementTop of Careaga FormationTpcKJfHorizontal distance alongseismic line, 2,000 ft increment(a)Uninterpreted(b)InterpretedArrows marking offset or truncated reflectors DCPPFile path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-21_Line_121.mxd; Date: 06/10/2014; User: Jereme Chandler, LCI; Rev.15-21AWD Line 121:(a) Uninterpreted and (b) Interpreted2011 ONSIPNotes:- Seismic line 121 awd fbm psdm 1 mix depth tvfagc.- Geology along topographic profile from Plate 1; see Plate 1 and Figure 6-1 for explanation of map units.
- Horizontal offsets are shown along a topographic profile above the seismic line.Pacific Gas and Electric CompanyFigureSeismic line in blueEXPLANATIONFault: solid where well located, dashed where approximately locatedTop of Careaga FormationTpcTop of Mesozoic basementKJfHorizontal distance along seismic line, 2,000 ft increment(a)Uninterpreted(b)InterpretedArrows marking offset or truncated reflectors File path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-23.mxd; Date: 06/26/2014; User: Alex Remar, LCI; Rev.1
!!!!!!!!!!!!!!!!!!!FAULTZONEEDNAFAULTZONELOSOSOS204 N240002800032000KJfmTmpeQlsQafTmoKJfmKJfmTovKJfmvTmpeTmoQls s sTmpmTmrQoaQcQal sQlsKJfmQaf sKJfmvKJfmvKJfm sKJfgQalTomQcKJfmKJfmKJfmvKJfmvKJfmvQal schKJfgQcTomQlsQoa sQlsQalQeKJfmvKJfmKJfmTomQoaKJfmv sKJfmQeQalQalKJfmv 04000800012000160001200016000138-149150-120°45'-120°45'35°15'35°15'Map projection and scale: WGS 84 / UTM Zone 10N,1:40,061µEXPLANATION
^_DCPP Cambria San Luis ObispoFigure extentKey Seismic Lines Imagingthe Los Osos Fault5-232011 ONSIP
+/-00.5 1mi.0 1 2kmPacificOceanHorizontal distance along seismic line,2,000 ft. incrementsVibroseis seismic reflection lineAWD seismic reflection lineNote: See Plate 1 for full list of geologic units and symbols.
!Pacific Gas and Electric CompanyFigure File path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-22.mxd; Date: 06/26/2014; User: Alex Remar, LCI; Rev.1
!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@llllllll°°°°°°47 36 14 38 76 43 48 47 24 45 15 65 47 32 15 25 25 18 35 50 55 45 25 30 50 20 29 30 70 60 40 35 35 38 50 50 35 45 50 70 85 60 50 25 20 80 48 60 30 65 45 40 47 72 35 26KJfgKJfm sKJfmQeKJfmvQlsKJfmvQalQalchKJfgQeQalTmpmQcQafQeQoaKJfmvQal sQsTomKJfmTomKJfmQlsQlsQeQeQalQesMap projection and scale: WGS 84 / UTM Zone 10N,1:28,000µ^_+/-00.5 1mi.00.5 1kmNotes:- See Plate 1 for explanation of geologic units and symbols.
For well names, see Figure 6-1.Vibroseis seismic reflection line Wells with picks for elevation of top ofMesozoic basementAWD seismic reflection line Horizontal distance along seismic line,2,000 ft incrementsPacificOceanFault: solid where well located, dashed whereapproximately located, short dashed where offset is less than contour interval, queried whereuncertainElevation of top of Mesozoic basement (ft)Plunging anticline
°!Pacific Gas and Electric CompanyFigureLocal structural high (+)Local structural low (-)
DCPPFile path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-24_Line_138_149.mxd; Date: 06/10/2014; User: Jereme Chandler, LCI; Rev.15-24AWD Line 138-149 Across the Los Osos Fault:(a) Uninterpreted and (b) Interpreted2011 ONSIPEXPLANATIONNotes:- Seismic line 138-149 - AWD FBM tvfagc.- Geology along topographic profile from Plate 1; see Plate 1 and Figure 7-1 for explanation of map units.
- Horizontal offsets are shown along a topographic profile above the seismic line.Pacific Gas and Electric CompanyFigureSeismic line in redFault: solid where well located,dashed where approximately locatedHorizontal distance alongseismic line, 2,000 ft increment(a)Uninterpreted(b)InterpretedArrows marking offset or truncated reflectors DCPPFile path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-25_Line_150.mxd; Date: 06/10/2014; User: Jereme Chandler, LCI; Rev.15-25AWD Line 150 Across the Los Osos Fault:(a) Uninterpreted and (b) Interpreted2011 ONSIPEXPLANATIONFault: solid where well located,dashed where approximately locatedNotes:- Seismic line 150 AWD FBM tvfagc.- Geology along topographic profile from Plate 1; see Plate 1 and Figure 7-1 for explanation of map units.
- Horizontal offsets are shown along a topographic profile above the seismic line.Pacific Gas and Electric CompanyFigureSeismic line in blueHorizontal distance alongseismic line, 2,000 ft increment(a)Uninterpreted(b)InterpretedArrows marking offset or truncated reflectors DCPPNotes:- Seismic line trimmed_204_north_2D_beam_50K_vibeonly_ poly_sl_stackagc_IEEE.- Geology along topographic profile from Plate 1; see Plate 1 and Figure 7-1 for explanation of map units.- Horizontal offsets are shown along a topographic profile above the seismic line.5-26Vibroseis Line 204 North:(a) Uninterpreted and (b) Interpreted2011 ONSIPPacific Gas and Electric CompanyFigureSeismic line in redEXPLANATIONFault: solid where well located, dashed where approximately locatedBase of KJfgHorizontal distance along seismic line, 2,000 ft increment(a)Uninterpreted(b)InterpretedArrows marking offset or truncated reflectors File path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-27.mxd; Date: 06/26/2014; User: Alex Remar, LCI; Rev.1
!!!!!!!!!!!!!!!!!!!!!ZONESANMIGUELITOFAULTSANLUISBAYFAULTFAULTZONESHORELINEUnnamedFault splaysRattlesnakesplayOlsonsplay 040008000120001600020000QswKJfQswQsQsKJfo KsQuQlsKJf KsQalQmQmTmoTmo KsQsTppsKJfm sQlsKJfTppgKJfmTppbTppsTmm KsTmodTmoKJfmTppgTovTmoQlsQmQalTmoQlsTmmTmpmQalPort SanLuis 04000 04000GreenPeak113114112-140-120°45'-120°45'35°10'35°10'Map projection and scale: WGS 84 / UTM Zone 10N,1:28,000µEXPLANATION
^_San Luis ObispoDCPPFigure extentKey Seismic Lines Imagingthe San Luis Bay Fault5-272011 ONSIP
+/-00.5 1mi.00.5 1kmAWD seismic reflection lineHorizontal distance along seismic line,2,000 ft incrementsPacificOceanNotes:- See Plate 1 for full list of geologic units and symbols.- Offshore geology from PG&E (2011).
!Pacific Gas and Electric CompanyFigure Notes:- Seismic line 113 AWD FBM PSDM 1 Mix Depth Tvfagc.- Geology along topographic profile from Plate 1; see Plate 1 and Figure 8-1 for explanation of map units.
- Horizontal offsets are shown along a topographic profile above the seismic line.5-28AWD Line 113:(a) Uninterpreted and (b) Interpreted2011 ONSIPPacific Gas and Electric CompanyFigureEXPLANATIONFault: solid where well located,dashed where approximately locatedReflector within basement rocksHorizontal distance alongseismic line, 2,000 ft increment(a)Uninterpreted(b)InterpretedArrows marking offset or truncated reflectorsDCPPSeismic line in red EXPLANATIONFault: solid where well located,dashed where approximately locatedTop of Mesozoic BasementNotes:- Seismic line 114_AWD_FBM_psdm_1_mix_depth_tvfagc.- Geology along topographic profile from Plate 1, see Plate 1 and Figure 8-1 for explanation of map units.
- Horizontal offsets are shown along a topographic profile above the seismic line.
5-29AWD Line 114:(a) Uninterpreted and (b) Interpreted2011 ONSIPPacific Gas and Electric CompanyFigureHorizontal distance along seismic line, 2,000 ft increment(a)Uninterpreted(b)InterpretedArrows marking offset or truncated reflectorsDCPPSeismic line in red File path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-30.mxd; Date: 06/10/2014; User: Alex Remar, LCI; Rev.15-30Geologic Cross Section A-A2011 ONSIPEXPLANATIONGeologic cross section J J J J^
_AAA'DCPP-120°45'-120°50'35°15'35°10'Location of geologic cross sectionGeologic Units024km+/-Note:See Figure 5-1 and Plate 1 for geologicmapping along cross section.Source: Seismicity data from Hardebeck (2014).Pacific Gas and Electric CompanyFigureSeismicity [M]2.50 - 3.500.00 - 0.490.50 - 0.991.00 - 1.491.50 - 1.992.00 - 2.49 File path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-31.mxd; Date: 06/24/2014; User: Alex Remar, LCI; Rev.15-31Geologic Cross Section B-B2011 ONSIPEXPLANATIONGeologic cross section J JSeismicity [M]0.00 - 0.490.50 - 0.991.00 - 1.491.50 - 1.992.00 - 2.49 J J^_BBB'DCPP-120°45'-120°50'35°15'35°10'Location of geologic cross sectionGeologic Units2.50 - 3.50 0 2 4km+/-Note: See Figure 5-1 and Plate 1 for geologicmapping along cross section.Source: Seismicity data from Hardebeck (2014).Pacific Gas and Electric CompanyFigure File path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-32.mxd; Date: 06/10/2014; User: Alex Remar, LCI; Rev.15-32Geologic Cross Section C-C'2011 ONSIPEXPLANATIONGeologic cross section J JSeismicity [M]0.00 - 0.490.50 - 0.991.00 - 1.491.50 - 1.992.00 - 2.49 J J^
_CC'DCPP-120°45'-120°50'35°15'35°10'Location of geologic cross sectionGeologic Units2.50 - 3.50024km+/-Notes: See Figure 5-1 and Plate 1 for geologicmapping along cross section.Source: Seismicity data from Hardebeck (2014).Pacific Gas and Electric CompanyFigure
??????????????0 1000-1000-2000
-3000
-4000
-5000 0 1000 2000 2000-1000-2000
-3000
-4000
-5000-6000-6000-7000-7000-8000 Depth (ft)
Scale: 1:24,000 Grid spacing 1,000 x 1,000 ft
No vertical exaggeration D D'South North Tmm Tmm Tmpm Tmo Tmo KJf KJf Tmod Tmod Tmor Tmor TmoSHORELINE FAULT Tmm Tmpm KJf Tmod Tmor TmoEXPLANATION Fault: solid where well located, dashed
where approximately located, queried
where uncertain Apparent dip Form line Franciscan Complex Obispo Formation Obispo diabase Monterey Formation Pismo Formation, Miguelito MemberObispo Formation, resistant tuff unit
?Location of geologic cross sections File path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-33_24kCrossSection_D-D.ai; Date: 06/26/2014; User: Matt Huebner, LCI; Rev.1 Figure Pacific Gas and Electric Company Geologic Cross Section D-D
'5-332011 ONSIP Scale: 1:24,000 Grid spacing 1,000 x 1,000 ft
No vertical exaggeration
???????????0 1000-1000-2000
-3000
-4000
-5000 0 1000 2000 2000-1000-2000
-3000
-4000
-5000-6000-6000-7000-7000-8000-8000 E E'Tmm Tmpm Tmo Depth (ft)
Fault: solid where well located, dashed where approximately located, queried
where uncertain Apparent dip Form line KJf Franciscan Complex Obispo Formation Tmod Obispo diabase Monterey Formation Pismo Formation, Miguelito Member TmorObispo Formation, resistant tuff unit
?Obispo Tuffaceous Siltstone TmofEXPLANATION Location of geologic cross sections File path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-34_24kCrossSection_E-E.ai; Date: 06/26/2014; User: Matt Huebner, LCI; Rev.1 Figure Pacific Gas and Electric Company Geologic Cross Section E-E
'5-342011 ONSIP Tmm Tmpm Tmo KJf Tmod Tmor Tmo Tmod TmofSHORELINE FAULT South North DCPP Scale: 1:24,000 Grid spacing 1,000 x 1,000 ft
No vertical exaggeration 0 1000-1000-2000
-3000 Depth (ft)
-4000
-5000 0 1000 2000 2000-1000-2000
-3000
-4000
-5000-6000-6000-7000-7000-8000-8000 F F'South North Tmm Tmpm Tmo KJf Tmod Tmor Tmm Tmo Tmo KJf KJf Tmor KJfSHORELINE FAULT Location of geologic cross sectionsFile path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-35_24kCrossSection_F-F.ai; Date: 06/26/2014; User: Matt Huebner, LCI; Rev.1 Tmm Tmpm KJf Tmod Tmor Tmo Fault: solid where well located, dashed where approximately located, queried
where uncertain Apparent dip Form line Franciscan Complex Obispo Formation Obispo diabase Monterey Formation Pismo Formation, Miguelito MemberObispo Formation, resistant tuff unit
?Figure Pacific Gas and Electric Company Geologic Cross Section F-F
'2011 ONSIPEXPLANATION 5-35????????????????????????
0-2000 2000 1000-4000-8000-12000 0-2000 2000 1000-4000-8000
-12000 0-2000 2000 1000-4000-8000-12000 0-2000 2000 1000-4000-8000
-12000?????0-2000 2000 1000-4000-8000-12000 0-2000 2000 1000-4000-8000
-12000 1 2 4 mi.0 S Grid spacing 2,000 x 2,000 ft No vertical exaggeration A A'B B'BC C'San Luis Bay Los Osos fault Edna C fault Shoreline fault fault???????Uplift and northward tilting
along range front above blind
tip of Los Osos fault ?
Honolulu-Tidewater San Miguelito Fault Zone
??File path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-36_32kFenceDiagrams.ai; Date: 06/10/2014; User: Matt Huebner, LCI; Rev.1 Figure Pacific Gas and Electric Company Structural Fence Diagram of the Irish Hills 5-362011 ONSIP Depth (ft)
Depth (ft)
Depth (ft) 0-2000 2000 1000-4000-8000-12000 0-2000 2000 1000-4000-8000
-12000-16000-16000-20000-20000-24000-24000-28000-28000-32000
-36000-40000 12 km-36000-40000-32000 4.4%0.2%3.4%8.7%7.3%1.3%6.7%0.7%-1.8%-4.7%3.5%-4.0%Los Osos faultEdna C faultEdna A faultEdna B faultAncenstral Shoreline fault (?)KJfKJfTmodTmodTmorTmorTmorTmoTmoTmoTmoTmoTmoTmoTmmTmmTmmTmpTmmKJfKJfKJfKJfKJfKJfKJf?????Scale: 1:24,000 Grid spacing 2,000 x 2,000 ft
No vertical exaggeration B BSouth North Bend in section (B
')Tmm Tmpm KJf Tmod Tmor Tmo Fault: solid where well located, dashed
where approximately located, queried
where uncertain Apparent dip Form line Franciscan Complex Obispo Formation Obispo diabase Monterey Formation Pismo Formation, Miguelito MemberObispo Formation, resistant tuff unit
?Location of geologic cross sections File path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-37_24kCrossSection_B-B.ai; Date: 06/26/2014; User: Matt Huebner, LCI; Rev.1 Figure Pacific Gas and Electric Company Geologic Cross Section B-B
Restored 5-372011 ONSIP Thickness (ft)EXPLANATION File path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-38.ai; Date: 06/10/2014; User: Alex Remar, LCI; Rev.1Pacific Gas and Electric Company FigureSandbox Model of a TranstensionalBasin Deformed by Transpression 5-382011 ONSIP (a) Analogue sandbox model of an extensional basin formed under left-lateral transtensional boundary conditions (top left), and subsequently deformed under right-lateral transpressional conditions (top right). Note the right-stepping en echelon pattern of the
normal faults formed during sinistral transpression, and development of lobate thrust faults along the margins of the extensional basin
system during the later phase of transpression.(b) Cross section through the final sandbox model (F-F'; location in upper right figure) showing a late-stage transpressional reverse
fault splaying upward from the principal displacement zone at the base of the model.
Source: Figures from Ustaszewski et al., (2005).
File path: S:\1005\034\QA_GIS\7_1_6_Report_Figures\Draft Report Figures\Figure_5-39.ai; Date: 06/10/2014; User: Alex Remar, LCI; Rev.1Pacific Gas and Electric Company FigureCross Sections Through Transpressionally Deformed Extensional Basin 5-392011 ONSIP Cross section through an analogue sandbox model of a transtensional basin subsequently deformed under transpressional boundary conditions. Note that late-stage thrust and reverse faults splay upward from the principal displacement zone at the base of the model that formed the root zone for the normal faults. Also note that the normal faults are locally cut and offset by
the late-stage reverse faults.
Source: Figures from Ustaszewski et al., (2005).
C C'B'B A'A