Fig. 5From: Stress and pore fluid pressure control of seismicity rate changes following the 2016 Kumamoto earthquake, JapanCoseismic stress fields of the largest foreshock and the mainshock of the Kumamoto earthquake. Coseismic stress fields at depths of (a) 5 km, (b) 10 km, and (c) 15 km. The pattern of coseismic stress changes fields is represented in the same way as in Fig. 4. The color scales show magnitudes of coseismic deviatoric stress changes. The stars are the same as in Fig. 2Back to article page