2004
DOI: 10.3133/ofr20041282
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Using twelve years of USGS refraction lines to calibrate the Brocher and others (1997) 3D velocity model of the Bay Area

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Cited by 17 publications
(26 citation statements)
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“…VSP and sonic log data provide measurements of Vp for the Franciscan Complex to depths up to 2.7 km (Majer et al, 1988;Newhouse et al, 2004;Brocher, 2005c). Laboratory measurements of Franciscan Complex rocks (Stewart and Peselnick, 1978), laboratory measurements for graywackes (Christensen and Mooney, 1995;Brocher and Christensen, 2001), and tomography velocities sample Franciscan Complex rocks at various depths up to 20 km (Beaudoin et al, 1996;Parsons and Zoback, 1997;Henstock and Levander, 2000;Hole et al, 2000;Boatwright et al, 2004;Catchings et al, 2004;Hauksson et al, 2004;Hardebeck et al, 2007).…”
Section: Franciscan Complex (Metagraywacke)mentioning
confidence: 98%
“…VSP and sonic log data provide measurements of Vp for the Franciscan Complex to depths up to 2.7 km (Majer et al, 1988;Newhouse et al, 2004;Brocher, 2005c). Laboratory measurements of Franciscan Complex rocks (Stewart and Peselnick, 1978), laboratory measurements for graywackes (Christensen and Mooney, 1995;Brocher and Christensen, 2001), and tomography velocities sample Franciscan Complex rocks at various depths up to 20 km (Beaudoin et al, 1996;Parsons and Zoback, 1997;Henstock and Levander, 2000;Hole et al, 2000;Boatwright et al, 2004;Catchings et al, 2004;Hauksson et al, 2004;Hardebeck et al, 2007).…”
Section: Franciscan Complex (Metagraywacke)mentioning
confidence: 98%
“…For the San Francisco Bay Area (SFBA), we use Version 08.3.0 of a 3D Bay Area velocity model developed by Boatwright et al (2004; http://earthquake.usgs.gov/research/ structure/3dgeologic/). Similar to the SCEC model, this 3-D velocity model is based on a structural and geological model of the region, which is converted to V p and then to V s .…”
Section: Basin Models In Northern Californiamentioning
confidence: 99%
“…The obtained velocity structure is comparable with additional velocity images derived from SFBR refraction experiments. Profiles AA′ and BB′ of Figure 8c coincide with portions of profiles AA′ and BB′ of Boatwright et al [2004]. Along profile AA′ the two velocity images both exhibit a strong low‐velocity volume from profile distance 0 to 20 km at depth ≲8 km, which envelopes the Loma Prieta rupture zone (see also Figure 18b).…”
Section: Discussionmentioning
confidence: 67%
“…This sense of velocity contrast at depth is seen in the y = 32.5 km, y = 42.5 km, and y = 52.5 km profiles in Figure 8a, and also in profile CC′ of Figure 8c. Profile CC′ has been taken to coincide with a portion of profile CC′ of Boatwright et al [2004], which contains velocity images derived from travel time tomography of several SFBR refraction experiments. The two sets of velocity profiles agree with the sense of velocity contrast across the SAF at both shallow (<5 km) and greater depth.…”
Section: Discussionmentioning
confidence: 99%