Project Abstract
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We have carried out a multi-faceted effort to improve the three-dimensional (3D) seismic velocity model for the region encompassing the San Jacinto fault zone (SJFZ) (Figure 1). P- and S-wave seismic velocity models have previously been determined for this region from separate inversions of body-wave arrival times by Allam and Ben-Zion (2012) for Vp and Vs and surface-wave dispersion data (from ambient noise) by Zigone et al. (2014) for Vs. These studies provided a starting point for our SCEC-supported work. The tasks that have been carried out consist of the following: (1) apply an effective automatic S-wave picker to an enlarged SJFZ waveform data set to provide data to further improve the sampling of the Vs structure; (2) develop ambient-noise surface-wave measurements at shorter and longer periods to provide increased constraint on the shallower and deeper structure, respectively, in the SJFZ region; (3) carry out joint body wave-surface wave inversions, including the addition of a substantial set of P-wave travel times from explosions to the earthquake dataset; (4) assess the validity of joint inversion models compared to the SCEC models by forward-modeling full-waveform data for a selected earthquakes. |