Fig. 11From: Characterized source model of the M7.3 2016 Kumamoto earthquake by the 3D reciprocity GFs inversion with special reference to the velocity pulse at KMMH16Comparison of the slip velocity functions for 2016 Kumamoto earthquake (this study, solid lines) and for 1995 Kobe earthquake (Matsushima and Kawase 2000, dotted lines). All STFs are centered to their peaks. Wider STFs are for lager SMGAs in both studiesBack to article page