Fig. 8From: Geomorphic features of surface ruptures associated with the 2016 Kumamoto earthquake in and around the downtown of Kumamoto City, and implications on triggered slip along active faultsSpatial relations of the NW-trending minor surface ruptures with aftershocks, focal mechanisms, and stress imparted from the Kumamoto main shock. a Aftershocks from the Japan Meteorological Agency catalog until September 18, 2016. b Focal mechanisms of the larger aftershocks determined from National Research Institute for Earth Science and Disaster Resilience (2016). c Coulomb stress change resolved onto NW-striking normal faults. d Coulomb stress change resolved onto NW-striking thrust faults. In both c and d, the source fault model of the Geospatial Information Authority of Japan (2016a) as gray rectangular is used for the stress calculation with apparent coefficient of friction 0.4 at a depth of 2.5 km. Receiver fault that Coulomb stress is resolved is shown as the red line on the beach ball and in the parentheses (strike/dip/rake) on each panel Back to article page