Poster #109, Stress and Deformation Over Time (SDOT)
Resolving Coseismic Stresses Using 3D Geodetic Imaging Data: Examples from the 2019 Ridgecrest Earthquake Sequence
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Poster Presentation
2021 SCEC Annual Meeting, Poster #109, SCEC Contribution #11136 VIEW PDF
rface deformation pattern in high spatial detail (at meter scale pixel resolution with decimeter accuracy) that can measure the full slip vector. Using this technique, we measured the 3D surface deformation and coseismic slip vectors every ~100 m along the faults that ruptured during the 2019 Ridgecrest earthquake sequence. From the coseismic surface slip vector data we then invert for the coseismic 3D stress tensor under the Wallace-Bott assumption that the observed slip vector is parallel to the shear stress. With estimates of the co-seismic stress state we will discuss the degree of stress heterogeneity along the rupture length, whether stresses rotate from the far-field towards the fault-zone and if there are any significant temporal changes of stress between the inter-, co- and post-seismic periods. Observational constraints of the spatiotemporal variation of the co-seismic stress state along ruptures will provide key initial conditions for physics-based dynamic rupture simulations, that will in turn provide more realistic estimates of ground motions and zones of distributed inelastic strain that are used as critical input for non-ergodic hazard calculations such as PSHA and PFDHA, respectively.
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