Group B, Poster #046, Seismology
The variable continuous bimaterial interface in the San Jacinto fault zone revealed by dense seismic array analysis of fault zone head waves
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Poster Presentation
2022 SCEC Annual Meeting, Poster #046, SCEC Contribution #12318 VIEW PDF
ther. The analysis reveals a >70 km long continuous bimaterial interface within the SJFZ with several deep northeast dipping fault segments. The northern SJFZ, for instance, locates ~7 km northeast of its surface expression at 18 km depth. P-wave velocity contrasts range from 0% to >15%, consistent with other bimaterial faults, and differ by a few % depending on fault-array azimuth, implying velocity contrast anisotropy. S-wave head waves and velocity contrasts are also imaged for the first time at the southern SJFZ, averaging to 2% (+/- 1.8%) in agreement with tomography results. The imaged geometry and continuity suggest the SJFZ initiated along remnant tectonic structures and translates to a rupture potential of M>7.2, i.e., the sizes of its largest paleo-earthquakes. The P and S contrasts, and their ratios, have important implications for earthquake rupture speed, mode, directivity and frictional heating along the SJFZ and other major faults globally.
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