Fig. 3From: Source rupture process of the 2016 central Tottori, Japan, earthquake (M JMA 6.6) inferred from strong motion waveforms a Comparison of observed waveforms (black) and synthetic waveforms (red). Maximum values are shown on the upper right hand corner of each waveform. b Contribution of slips on R1 (broken blue, Fig. 2a) and on R2 (magenta, Fig. 2a) to synthetic waveforms. Orange bars denote the time when the contribution of R2 to synthetic waveforms is largeBack to article page