Fig. 4From: Source process of the 2016 Kumamoto earthquake (Mj7.3) inferred from kinematic inversion of strong-motion recordsTotal slip distribution of the first-step inversion using 0.05–0.5 Hz band-pass strong-motion data. The two columns on the west side of the fault model were trimmed following the criteria by Somerville et al. (1999)Back to article page