HIGHLIGHTS
SUMMARY
In Fig 3, the authors show the evolution of change of fault stability for fault plane solutions of the largest earthquake (29 August 2020) (see "Methods") with and without pore pressure computed using hydraulic diffusivity (C) and fault friction (μ) values appropriate for intraplate settings. By definition, shear failure of a fault is promoted if the change of fault stability is positive and it is impeded when fault stability is negative. For the steep fault striking 265° with an oblique normal sense of slip (Supplementary Table S2 and Fig 2a), the authors find that the . . .
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