Fig. 6From: Source rupture processes of the 2016 Kumamoto, Japan, earthquakes estimated from strong-motion waveformsComparison of observed waveforms (black), synthetic waveforms produced by the curved fault model (red), and synthetic waveforms produced by the single fault plane model (blue) in the analysis of the M 7.3 event. The maximum values are shown on the upper right of each waveformBack to article page