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Fig. 2 | Earth, Planets and Space

Fig. 2

From: Coulomb stress change on inland faults during megathrust earthquake cycle in southwest Japan

Fig. 2

Coseismic stress changes on an inland fault with varying strike and dip. The inland fault is located 150 km from the upper-edge of the megathrust fault. The rake of the dextral fault, sinistral fault, reverse fault, and normal fault for calculating the shear stress and \(\Delta {\text{CFS}}\) are 180°, 0°, 90°, and − 90°, respectively. a Shear stress change, b normal stress change, c\(\Delta {\text{CFS}}\) with an apparent friction coefficient of 0.1, and d\(\Delta {\text{CFS}}\) with an apparent friction coefficient of 0.4

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