Poster #122, Stress and Deformation Over Time (SDOT)
Triggered and Spontaneous Slow Slip Transients on the Anza Segment of the San Jacinto Fault Zone, Southern California
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Poster Presentation
2020 SCEC Annual Meeting, Poster #122, SCEC Contribution #10590 VIEW PDF
ents with coplanar burst-type repeating earthquakes and off-fault microseismicity. These observations include newly detected triggered slow slip transients following the June 10, 2016 Mw 5.2 Borrego Springs earthquake and the April 4, 2020 Mw 4.9 earthquake. Slow slip geometries defined by burst-type repeating earthquakes are consistent with strain change observations and reveal multiple active planes both on and off of the triggering earthquake fault. We conclude that burst-type repeating earthquakes, similar to low-frequency earthquakes, are useful indicators of slow slip transients and can reveal faulting complexities during slow slip. Further, we identify the first evidence of spontaneous slow slip in this region from burst-type repeating earthquake families on two minor faults in 2015. Taken together, our observations support a model where deep microseismicity is located in a transitional region at the bottom of the seismogenic zone with spatially heterogeneous frictional properties that produces frequent slow slip transients.
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