Figure 9. Coulomb stress changes due to the 2016 Mw5.9 earthquake resolved onto (a) the left-lateral faults parallel to the 2022 rupture plane and (b) onto the 2022 fault plane of the finite fault model of Wang et al. (Figure 3). We implemented a simple uniform slip model of the NW-striking blind thrust for the 2016 earthquake based on the USGS CMT and Wells and Coppersmith (1994) empirical relation. Credit: Shinji Toda

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Figure 9. Coulomb stress changes due to the 2016 Mw5.9 earthquake resolved onto (a) the left-lateral faults parallel to the 2022 rupture plane and (b) onto the 2022 fault plane of the finite fault model of Wang et al. (Figure 3). We implemented a simple uniform slip model of the NW-striking blind thrust for the 2016 earthquake based on the USGS CMT and Wells and Coppersmith (1994) empirical relation. Credit: Shinji Toda

Figure 9. Coulomb stress changes due to the 2016 Mw5.9 earthquake resolved onto (a) the left-lateral faults parallel to the 2022 rupture plane and (b) onto the 2022 fault plane of the finite fault model of Wang et al. (Figure 3). We implemented a simple uniform slip model of the NW-striking blind thrust for the 2016 earthquake based on the USGS CMT and Wells and Coppersmith (1994) empirical relation. Credit: Shinji Toda

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