Figure 10. The maximum Coulomb stress imparted by both 2016 and 2022 events for (a) WNW-striking left-lateral faults, and (b) NW-trending thrust faults at a depth range of 5-15 km. The finite fault model by Wang et al. (Figure 3) is used for the 2022 earthquake stress transfer. Credit: Shinji Toda.

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Figure 10. The maximum Coulomb stress imparted by both 2016 and 2022 events for (a) WNW-striking left-lateral faults, and (b) NW-trending thrust faults at a depth range of 5-15 km. The finite fault model by Wang et al. (Figure 3) is used for the 2022 earthquake stress transfer. Credit: Shinji Toda.

Figure 10. The maximum Coulomb stress imparted by both 2016 and 2022 events for (a) WNW-striking left-lateral faults, and (b) NW-trending thrust faults at a depth range of 5-15 km. The finite fault model by Wang et al. (Figure 3) is used for the 2022 earthquake stress transfer. Credit: Shinji Toda

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