Calculations, via Coulomb 3.3 (Toda et al., 2011), of the stress imparted by the magnitude-6.4 earthquake to major mapped faults (left), and to the faults on which past earthquakes struck (right). The focal mechanisms in the upper right panel are from the Global CMT catalog, from 1976 to 2022. Here, we assume the fault friction is 0.4.

Calculations, via Coulomb 3.3 (Toda et al., 2011), of the stress imparted by the magnitude-6.4 earthquake to major mapped faults (left), and to the faults on which past earthquakes struck (right). The focal mechanisms in the upper right panel are from the Global CMT catalog, from 1976 to 2022. Here, we assume the fault friction is 0.4.

Calculations, via Coulomb 3.3 (Toda et al., 2011), of the stress imparted by the magnitude-6.4 earthquake to major mapped faults (left), and to the faults on which past earthquakes struck (right). The focal mechanisms in the upper right panel are from the Global CMT catalog, from 1976 to 2022. Here, we assume the fault friction is 0.4.

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