2022
DOI: 10.1029/2021jb023331
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Vertical Postseismic Deformation of the 2019 Ridgecrest Earthquake Sequence

Abstract: On July 4-5, 2019, the Mw6.4 and Mw7.1 Ridgecrest earthquake sequence ruptured a geometrically complex, 50 km long, system of faults within the Eastern California Shear Zone (ECSZ). The ECSZ is situated eastward and parallel to the San Andreas Fault System (SAFS) and accommodates approximately 20% of the Pacific and North American plate boundary motion, while the SAFS accounts for 80% (

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Cited by 5 publications
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“…1). We see postseismic uplift around the 1999 Hector Mine, 1992 Landers [22], and uplift and subsidence associated with 2019 Ridgecrest earthquake [24]. Most of these large-scale natural processes appear to be stable in this study time-span (temp.…”
Section: Estimating Spatially and Temporally Varying Vertical Land Mo...mentioning
confidence: 68%
“…1). We see postseismic uplift around the 1999 Hector Mine, 1992 Landers [22], and uplift and subsidence associated with 2019 Ridgecrest earthquake [24]. Most of these large-scale natural processes appear to be stable in this study time-span (temp.…”
Section: Estimating Spatially and Temporally Varying Vertical Land Mo...mentioning
confidence: 68%