Fig. 6From: Stress and pore fluid pressure control of seismicity rate changes following the 2016 Kumamoto earthquake, JapanCoulomb failure stress changes (ΔCFS) by the largest foreshock and the mainshock. Distributions of ΔCFS at depths of (a) 5 km, (b) 10 km, and (c) 15 km. The color scales show values of ΔCFS (which are truncated outside the region from − 0.1 to 0.1). The stars, the light green rectangles, the triangles, the black dahsed lines, and the grey lines are the same as in Fig. 2Back to article page