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PSUsing Petroleum Industry 3D Surveys to Improve Understanding of Active Faults: The Palos Verdes Fault in San Pedro Bay, California*
By
Andrew W. Rigor1, Mark R. Legg2, Robert J. Mellors1, and Robert D. Francis3
Search and Discovery Article #40088 (2003)*Adapted for online presentation from award-winning poster at Student Expo, Norman, OK, March, 2003.1San Diego State University ([email protected])
2Legg Geophysical
1California State University Long Beach
AbstractLarge earthquakes
on the Palos Verdes fault may be destructive to the nearby urban areas of the
densely populated Los Angeles Basin. We interpret an industry 3D seismic survey
(244 km2, CDP spacing 24.6 m inline, 50.3 m cross-line), and process
and interpret three intersecting shallow 2D profiles (16 channel, 0.95 s depth,
3.125 m CDP spacing), to map the shallow geometry (<3.0 s two-way travel 
time
)
of the fault zone in San Pedro Bay. Several reflectors, tied to known
stratigraphic boundaries using well logs, provide timing of interpreted features
that are used to improve understanding of the fault activity and associated
seismic hazard.
We observe five
distinct fault segments in the area of the 3D survey. Each segment consists of
one primary strand that is near vertical to at least 3.0 s two-way travel time,
and one to five secondary strands forming a zone that varies from 700-2400 m
width. Several of these fault strands break latest
Quaternary sediment and are associated with bathymetrically observed deformation
at the surface. Deformation character at fault bends is consistent with a
right-slip dominated fault zone. Seismic reflections of growth and no-growth
sequences above anticlines to the west of the fault and in the Quaternary
deposits of the Wilmington graben to the east of the fault are imaged in the
2D surveys. These alternating styles in
vertical deformation may be associated with lateral movement of sedimentary
sequences along bends in the main fault strand.
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(Complete captions accompany full-size images and follow text.)
Click here to view sequence of Figure4(a), (b), and (c).
Click here to view sequence of Figure 6(a), (b), (c), (d), and (e).
3D Seismic Reflection Data (Figure 2)
2D Seismic Reflection Data (Figure 3)
The Palos Verdes fault zone has a general northwest trend (Figures 1 and 2). Bends in the fault are associated with bathymetric changes; similarly, there are topographic changes along the Newport-Inglewood and Whittier faults, the other two major right-slip faults of the Los Angeles Basin.. The fault zone with its pop-up structure includes multiple fault strands. It separates the study area into two distinct seismic characters--Palos Verde anticlinorium to the west and Wilmington “graben” to the east (Figures 1, 2, and 3).
Anticlines within the study area are the San Pedro Bay anticlinorium and the “Beta ear” anticline west of the fault (Figure 6). Also west of the fault are the toe of the Palos Verdes Hills anticlinorium (in the north) and the underlying basement ridge. East of the fault is the Wilmington “graben,” with the THUMBS –Huntington Beach fault at the northeast edge of the study area and the main Beta oilfield monocline along the restraining segment of the Palos Verdes fault. A broad anticline, perpendicular to the fault, with associated growth during the Pliocene, may indicate the initiation of right-slip motion along the fault zone (Figure 7).
The narrow, tilted wedge of Quaternary strata southwest of the fault is generally too shallow to be effectively imaged with the 3D data. However, lines from 2D seismic data show the approximate location of the Quaternary wedge of sediments overlying the Palos Verdes Hills and San Pedro Bay anticlinoria, the Palos Verdes fault zone, and the Wilmington “graben” (Figures 8 and 9). This growth wedge and the monocline east of the fault are variable along strike; they may reflect uplift that formed as sediments were translated into the restraining bend.
3D data provided by Chevron-Texaco. Research funded by Southern California Earthquake Center.
Figure 1. Index map. The box on the inset map shows the location of the Palos Verdes fault and study area. The polygon shows the area of the 3D seismic data. Lines in violet show the 2D seismic profile locations. Mapped faults are in red. Note changes in bathymetry associated with bends in the Palos Verde fault (PVFZ). Similarly, the topography changes along the Newport-Inglewood ((NIFZ) and Whittier (WF) faults, the other two major right-slip faults of the Los Angeles Basin (LA Basin).
Figure 2.
Chair-cut visualization of Beta oil field 3D survey, cut at line 120, CDP 650, and
Figure 3. A
fence diagram of the locations of three 2D lines on top of the 1436-1492
ms 3D
Figure
4(a-c). Beta 3D seismic
Figure 5.
The location of the segments and features of the Palos Verdes fault
through the Beta 3D survey area. Green lines indicate the locations of
the three 16-channel seismic lines; background is a Figure 6(a-e). Individual cross-sections through segments A through E are labeled A-A’ through E-E’ and shown with interpreted faults and horizons. Anticlines within this survey are the San Pedro Bay anticlinorium (SPBA) and the “Beta ear” anticline to the west of the fault. Additionally to the west of the fault is the toe of the Palos Verdes Hills anticlinorium (PVHA) in the north and the underlying basement ridge. The latter is most likely a remnant Miocene bathymetric high at the peak of a tilted crustal block due to Borderland extension and rotation. To the east of the fault is the Wilmington “graben” with the THUMBS –Huntington Beach fault at the northeast edge of the survey and the main Beta oilfield monocline along the restraining segment (c) of the Palos Verdes fault. Figure 7. A broad anticline, perpendicular to the fault, below Pliocene horizon “C-2,” with associated growth through “C-top,” may be an indicator of initiation of right-slip motion along the fault zone. Color indicates depth to horizon “C-2.” Figure 8(a-b). Close-ups of 300 ms of 2D data from (a) line 80a, above, and (b) 81, below, have been annotated to show approximate location of the Quaternary wedge of sediments overlying the Palos Verdes Hills and San Pedro Bay anticlinoria (unconformity in green), the Palos Verdes fault zone (PVF), and the Wilmington “graben.” The narrow tilted wedge of Quaternary strata lying to the southwest of the fault is generally too shallow to be effectively imaged with the 3D data; note line 80a roughly corresponds to cross-section D-D’ (Figure 6(d)). This growth wedge and the monocline to the east of the fault appear variable along strike and may be due to uplift created as sediments have been recently translated into the restraining bend. Figure 9. 2-D, E-W seismic line 81 that extends across and beyond the study area. The Palos Verdes fault zone (PVF) is characterized by change in character across it, as well as the development of the Quaternary wedge highlighted in Figure 8(b).
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Figure 1.
Index map.
Figure 2.
Chair-cut visualization of Beta oil field 3D survey, cut at line 120,
CDP 650, and 
Figure 3. A
fence diagram of the locations of three 2D lines on top of the 1436-1492
ms 3D 
Figure
4(a-c). Beta 3D data 
Figure 5.
The location of the segments and features of the Palos Verdes fault
through the Beta 3D survey area. 
Figure
6(a-e). Individual cross-sections through segments A through E are
labeled A-A’ through E-E’ and shown with interpreted faults and horizons.
Figure 7. A
broad anticline, perpendicular to the fault, below Pliocene horizon
“C-2.”
Figure
8(a-b). Close-ups of 300 ms of 2D data from (a) line 80a, above, and (b)
81, below, have been annotated to show approximate location of the
Quaternary wedge of sediments overlying anticlinoria, fault zone, and
graben.
Figure
9. 2-D, E-W seismic line 81 that extends across and beyond the study
area.
