Group A, Poster #129, Fault and Rupture Mechanics (FARM)
The role of sediments and fault damage on the 2019 Ridgecrest earthquake: a rupture impediment and/or ground motion amplifier?
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Poster Presentation
2022 SCEC Annual Meeting, Poster #129, SCEC Contribution #11944 VIEW PDF
2021), and damage zones of Qiu et al. (2021). We also consider past-seismicity-caused initial stress heterogeneity, using our recent method of Oral et al. (2022) and catalogued foreshocks. Our findings are: 1) Sedimentary layers with or without damage slightly affect the rupture speed, whereas a low background stress can be a sufficient factor to explain the observed slow rupture; 2) Sedimentary layers amplifies fault slip and consequent ground motion, counterbalancing the damping effect of a slower rupture; 3) A simple sub-shear bilateral rupture model well captures the observed ground motion directivity. We plan to expand our study on other areas in California with different fault zone properties, to identify whether the damage effect in Ridgecrest is a paradigm or unusual for the regional seismic hazard.
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