Fig. 3From: Source process of the 2016 Kumamoto earthquake (Mj7.3) inferred from kinematic inversion of strong-motion recordsComparison of the observed velocities (Obs.), the synthetic velocities for the derived model (Inv.), and the synthetic velocities for the reference (initial) model (Ref.) of moderate earthquakes (0.3–1.0 Hz). The number at the upper right of each wave indicates the maximum amplitude of the observed waveforms. a S1 event at all stations. Time since the event origin is shown. b Zoomed view of KMM008. c S3 event at KMMH16. Waveforms in this panel are aligned to P-wave arrival to compare the S–P timeBack to article page