Fig. 12From: Stress and pore fluid pressure control of seismicity rate changes following the 2016 Kumamoto earthquake, JapanTheoretical estimates of increases in pore fluid pressure due to the Kumamoto earthquake at depths of (a) 5 km, (b) 10 km, and (c) 15 km. The color scales of symbols show overpressure coefficients of upper limits of theoretical increases in pore fluid pressure under the undrained condition (with B = 1). The red circles denote the evaluation points, where we observed significant increases in C after the mainshock. The grey rectangles are the same as in Fig. 8Back to article page