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Metadata
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ID
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L-1-91-NC
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Abstract
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Chief Scientists: Pat Hart, Jill McCarthy. Geophysical data
(3dot5khz, 12khz, uniboom, airgun, airgunmonitor) of field
activity L-1-91-NC in San Francisco Bay from 09/03/1991 to
09/20/1991
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Project/Theme
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Bay Area Seismic Imaging Experiment (BASIX)
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Chief Scientist
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Pat Hart
Jill McCarthy
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Activity Type
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Geophysical
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Platform
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Samuel Phillips Lee
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Area of Operation
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San Francisco Bay
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Location map
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Bounding Coordinates
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38.11173
-123.52004 -121.70993
37.20842
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Dates
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09/03/1991 (JD 246) to 09/20/1991 (JD 263)
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Analog Materials
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list
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Index map
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Crew
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Al McClenghan
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Ship Captain
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Chris Poppe
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Chief Mate, USGS Western Region
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Bill Lafleur
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Chief Engineer, USGS Western Region
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Jill McCarthy
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Chief Scientist, USGS Western Region
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Kevin O'Toole
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Mechanical Technician, USGS Western Region
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Walt Olson
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Mechanical Technician, USGS Western Region
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Larry Kooker
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Electronics Technician, USGS Western Region
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Bill Robinson
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Electronics Technician, USGS Western Region
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Jim Vaughan
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Electrical Engineer, USGS Western Region
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Dave Hogg
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Electronics Technician, USGS Western Region
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Kaye Kinoshita
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Navigator, USGS Western Region
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George Knudson
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Mechanical Technician, Fairfield
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Steve Higgins
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Electronics Technician, Fairfield
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Mike Pawlik
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Electronics Technician, Fairfield
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Tom McEvilly
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Geophysicist, University of California, Lawrence Berkeley Laboratories
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Pat Hart
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Geophysicist, USGS Western Region
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Jon Childs
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Geophysicist, USGS Western Region
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Kevin Furlong
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Geophysicist, Pennsylvania State University
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Terry Proffer
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Geophysicist, Haliburton Geophysicist.
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Pat McClellan
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Geophysicist, City Of San Leandro
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Mike Marlow
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Watchstander, USGS Western Region
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Kathy Furlong
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Unspecified Investigator, Pennsylvania State University
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Kate King
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Unspecified Investigator, CNN
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Rick Blackbird
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Unspecified Investigator, CNN
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Chris Vincent
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Unspecified Investigator, CNN
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Gordon Smith
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Ship Captain, David Johnston
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Mark McLaughlin
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Unspecified Investigator, David Johnston
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Tom Parsons
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Unspecified Investigator, Stanford University - David Johnston
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Michael Hamer
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Navigator, David Johnston, USGS Western Region
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Roberto Anima
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Ship Captain, Fast Eddy, USGS Western Region
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Shawn Dadisman
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Unspecified Investigator, Fast Eddy, USGS Western Region
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Armando Buciaga
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Unspecified Investigator, Fast Eddy, USGS Western Region
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Tom Chase
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Ship Captain, Chase Boat, USGS Western Region
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Pete Dartnell
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Unspecified Investigator, Chase Boat, USGS Western Region
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Roy Kiesling
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Vol. Unspecified Investigator, Chase Boat, USGS Western Region
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Greg Gabel
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Ship Captain, Caltrans
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Holly Ryan
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Unspecified Investigator, Caltrans
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David Verdonck
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Geophysicist, Pennsylvania State University, LLL
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Dennis Mann
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Ship Captain, Revenge, USGS Western Region
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Ray Sliter
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Unspecified Investigator, Revenge, USGS Western Region
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Joe Svitek
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Unspecified Investigator, Revenge, USGS Western Region
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Rich Clymer
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Unspecified Investigator, Mako, USGS Western Region
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Pat Williams
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Unspecified Investigator, Mako, USGS Western Region
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Peter Barnes
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Ship Captain, R/V Estero, USGS Western Region
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Erik Gize
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Unspecified Investigator, R/V Estero, USGS Western Region
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Jean Riordan
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Unspecified Investigator, USGS Western Region
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Norman Maher
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Unspecified Investigator, USGS Western Region
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Vicky Goetcheus
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Unspecified Investigator, USGS Western Region
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Dave Scholl
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Geophysicist, USGS Western Region
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Eleni Karageorgi
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Unspecified Investigator, Lawrence Berkeley Laboratories
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Joel Rosenbaum
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Photographer, Vacaville Reporter
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Robert Reed
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Unspecified Investigator, Vacaville Reporter
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George Thompson
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Geophysicist, Stanford University
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Ben Page
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Geophysicist, USGS Western Region
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David McMahon
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Unspecified Investigator, BC&DC
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Doug Prose
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Photographer, USGS Western Region
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Nina Luttinger
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Photographer, USGS Western Region
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Tracy Vallier
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Geologist, USGS Western Region
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Andy Michael
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Geophysicist, USGS Western Region
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Stephanie Ross
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Navigator, USGS Western Region
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Diana Collins
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Unspecified Investigator, USGS Western Region
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June Matsueyda
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Unspecified Investigator, USGS Western Region
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Equipment Used
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3dot5khz
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12khz
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uniboom
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airgun
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airgunmonitor
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Purpose
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Furlong and others (1989) proposed the possibility that the network
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of faults that bound the San Francisco Bay Area are linked structurally and
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are all part of an evolving fault system. To test the Furlong and others (1989)
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model and to obtain fundamental information on the crustal structure and fault
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geometries that underlie the San Francisco Bay Area, the USGS, in conjunction
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with the University of California, Stanford University, Pennsylvania State
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University, and Lawrence Berkeley Laboratory, conducted a major seismic
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reflection investigation in the fall of 1991 utilizing the marine waterway
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system that dissects the Bay Area. This study, known as the Bay Area Seismic
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Imaging Experiment (BASIX) consisted of three complementary seismic
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reflection and refraction profiling methods: high resolution seismic reflection
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profiling, wide-angle reflection/refraction profiling, and multichannel
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seismic profiling. The high-resolution, shallow penetration data were
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acquired to constrain near-surface faulting, while the wide-angle reflection/
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refraction data were acquired to constrain the deep-crustal velocity
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structure of the crust. (Open-File Report 93-301).
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Information to be Derived
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Three complementary seismic reflection and refraction profiling
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methods: high resolution seismic reflection profiling, wide-angle
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reflection/refraction profiling, and multichannel seismic profiling. The
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high-resolution, shallow penetration data were acquired to constrain
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near-surface faulting, while the wide-angle reflection/refraction data were
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acquired to constrain the deep-crustal velocity structure of the crust.
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(Open-File Report 93-301).
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Summary
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A total of 140 km of multichannel reflection data were acquired across
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the San Francisco Bay Area during 14 nights of profiling. Although each night
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of profiling was assigned a different line number, several of the lines overlap
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and they were thus processed together as merged profiles. All totaled, there
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were four distinct segments to the experiment. The first segment began in
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the Sacramento River near Rio vista and proceeded west through Honker, Suisun,
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and San Pablo Bays (lines 101 through 110). The next two segments ran north-
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south from Richmond to Angel Island (line 113), and from the Bay Bridge to
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just north of the San mateo Bridge (line 111). The fourth and final segment
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began in the vicinity of Alcatraz Island and extended west underneath the
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Golden Gate Bridge, 6 km into the open waters of the Pacific (lines 201-202).
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60 to 118 Telseis receivers were moored to the edge of the dredged shipping
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channel at 100 to 200 m intervals for a fixed spread of 6 to 12 km in length.
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Each day the receiver array was repositioned, and each night the S.P. Lee
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steamed along the hydrophone array, with its airgun array firing.
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The day-to-day small-boat operations began first with the retrieval of the
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Telseis instruments deployed the previous day. This process utilized a fleet
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of 4-5 small boats that ranged in size from 6 to 15 m. Once retreived, the
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instruments were brought back to the S.P. Lee for recharging. The R.V. David
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Johnston trailed behind these small vessels and recovered the associated buoys
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and anchors. The Johnston also recorded navigational fixes, which were
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required in order to check for possible drift of the instrument sites during
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the night; although anchors were used to maintain instrument position, currents
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were strong enough in a few areas to move the anchors between deployment and
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retrieval.
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Once the instrument retrieval was complete, the Johnston would begin laying
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out the next line segment. A GPS and Del Norte triangulation system were used
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to measure the 100- or 200-m distance separating instrument sites. The
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receiver line was positioned so as to minimize bends in the profile and to
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keep the buoys out of the active shipping channel. At each site, anchors
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were deployed and navigation fixes were taken; the anchored sites were marked by orange buoys. The smaller boats followed behind and clipped the recharged
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Telseis units with cabled hydrophones to these buoys. The hydrophones were
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weighted so as to minimize movement on the seafloor.
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The final phase of operation was airgun profiling. Each night the S.P. Lee
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acquired approximately 24 km of reflection data by looping through the
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receiver array twice. Along 10 of the 13 multichannel lines the S.P. Lee fired
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the airgun array while steaming first from east to west and then, reversing
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course, duplicated the line by steaming from west to east, further doubling
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the number of airgun shots available for stacking of the seismic signal.
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In addition to the 13 reflection lines acquired in San Francisco Bay and the
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Golden Gate region, the airgun array on the S.P. Lee was used primarily as a
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seismic source for wide-angle profiles recorded along three other lines: the
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N-S trending line OBS1 in San Francisco Bay; a short transit leg, line TR1
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SW of the Golden Gate; and the E-W trending line OBS2 on the continental margin.
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Lines OBS1 and OBS2 were obtained along two separate deployment of 6 USGS ocean bottom seismometers (OBS) deployed by investigators from the USGS Branch of
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Atlantic Marine Geology and Woods Hole Oceanographic Institution. The shot
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interval along line 112/OBS1 was 50 m. The shot interval for lines TR1 and
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OBS2 was approximately 75 m. Line OBS2 was located coincident to seismic
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reflection line 13 of Lewis (1990) in order to provide deep structural control
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on the continental margin west of the San Andreas fault.
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Publications
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Anima, R.J., Williams, Patrick L., and McCarthy, J., 1992, High-resolution marine
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seismic reflection profiles across East Bay faults, in Galehouse, Jon S., ed.,
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Programs and abstracts of the Second conference on Earthquake hazards in the
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eastern San Francisco Bay area: California Division of Mines and Geology Special
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Publication, v. 113, p. 4.
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Hart, P.E., Clymer, R.W., and Karageorgi, E.D., 1992, Geometry of the San Francisco
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Bay area faults; preliminary results from BASIX, in Galehouse, Jon S., ed.,
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Programs and abstracts of the Second conference on Earthquake hazards in the
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eastern San Francisco Bay area: California Division of Mines and Geology Special
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Publication, v. 113, p. 30.
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McEvilly, T.V., and McCarthy, Jill, 1992, BASIX; the Bay Area Seismic Imaging
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Experiment report, in Galehouse, Jon S., ed., Programs and abstracts of the Second
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conference on Earthquake hazards in the eastern San Francisco Bay area: California
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Division of Mines and Geology Special Publication, v. 113, p. 47.
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McCarthy, Jill, and Hart, Patrick E., 1993, Data report for the 1991 Bay area
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seismic imaging experiment (BASIX): U.S. Geological Survey Open-File Report 93-0301,
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26 p.
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Hart, P., McCarthy, J., Karageorgi, E., and McEvilly, T., 1993, Seismic reflection
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profiling in the San Francisco Bay area; the 1991 Bay Area Seismic Imaging Experiment
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(BASIX): Geological Society of America Abstracts with Programs, v. 25, no. 6,
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p. 417-418.
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McCarthy, J., Hart, P., Karageorgi, E., and McEvilly, T., 1993, Seismic profiling across
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an evolving transform margin; results from the 1991 Bay Area Seismic Imaging eXperiment
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(BASIX): Geological Society of America Abstracts with Programs, v. 25, no. 6, p. 310.
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Brocher, Thomas M., McCarthy, Jill, Hart, Patrick E., Holbrook, W. Steven, Furlong, Kevin P.,
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McEvilly, Thomas V., Hole, John A., and Klemperer, Simon L., 1994, Seismic evidence for a
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lower-crustal detachment beneath San Francisco Bay, California: Science, v. 265, no. 5177,
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p. 1436-1439.
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Childs, J.R., Hart, P.E., McCarthy, J., and Marlow, M.S., 1994, High-resolution
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seismic-reflection studies of submerged fault zones throughout the San Francisco Bay
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area: American Geophysical Union Eos, Transactions, v. 75, no. 44, Supplement, p. 684.
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McCarthy, J., Hart, P.E., Anima, R., Oppenheimer, D., and Parsons, T., 1994, Seismic
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evidence for faulting in the western Sacramento Delta region, Pittsburg, California:
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American Geophysical Union Eos, Transactions, v. 75, no. 44, Supplement, p. 684-685.
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McCarthy, J., Hart, P.E., and Oppenheimer, D., 1995, High angle faulting in western
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Sacramento Delta region, Pittsburg, California: American Association of Petroleum
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Geologists Bulletin, v. 79, no. 4, p. 592.
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Parsons, Tom, McCarthy, Jill, and Hart, P.E., 1994, The nature of lower crustal reflectors
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beneath San Francisco Bay, California: American Geophysical Union Eos, Transactions, v. 75,
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no. 44, Supplement, p. 643.
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Williams, P.L., McEvilly, T.V., Anima, R., McCarthy, J., Nakata, T., Okamura, M., and
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Shimazaki, K., 1993, Fault activity, geometry, and recurrence behavior at the junction of
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the Rodgers Creek and Pinole faults, California: American Geophysical Union Eos,
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Transactions, v. 74, no. 43, Supplement, p. 411.
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Holbrook, W. Steven, Brocher, T.M., McCarthy, Jill, Hole, J.A., and ten Brink, U.S., 1994,
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Crustal structure beneath the San Francisco Bay Block and Central California continental
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margin: American Geophysical Union Eos, Transactions, v. 75, no. 44, Supplement, p. 664.
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Pope, D.C., Brocher, T.M., McCarthy, J., Karageorgi, E.D., and Holbrook, W.S., 1993, Comparison
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of recording technology for onshore-offshore seismic profiling of continental margins; examples
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from BASIX: American Geophysical Union Eos, Transactions, v. 74, no. 43, Supplement, p. 445.
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Brocher, Thomas M., McCarthy, Jill, and Holbrook, W. Steven, 1996, Imaging the transform
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plate boundary in the San Francisco Bay area, California: Geological Society of America
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Abstracts with Programs, v. 28, no. 7, p. 216.
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Brocher, Thomas M., and Moses, Michael J., 1993, Onshore-offshore wide-angle seismic
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recordings of the San Francisco Bay Area Seismic Imaging Experiment (BASIX): the five-day
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recorder data: U.S. Geological Survey Open-File Report 93-276, 89 p.
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Got Help?
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For L-1-91-NC, we would appreciate any information on -- information to be derived, equipment used, information specialist, organization, ports, publications, purpose, summary.
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