Fig. 2From: Coulomb stress change on inland faults during megathrust earthquake cycle in southwest JapanCoseismic 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 0.4Back to article page