Fig. 13From: Rupture process of the main shock of the 2016 Kumamoto earthquake with special reference to damaging ground motions: waveform inversion with empirical Green’s functionsComparison of the observed and synthetic velocity waveforms (0.2–2 Hz) at the distant stations. The locations of the stations are shown in Fig. 1. These stations were not used in the inversion analysis. The black traces are the observed waveforms. The red traces are the synthetic waveforms. The Case 1 slip model was usedBack to article page