Fig. 2From: 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) for Case 1. The gray and black traces show the observed waveforms. The black traces correspond to the 15-s time sections used in the waveform inversion. The red traces show the synthetic waveformsBack to article page