Fig. 5From: Rupture process of the 2018 Hokkaido Eastern Iburi earthquake derived from strong motion and geodetic dataObserved and synthetic borehole and ground surface waveforms of EW components at station IBUH03. Locations, velocity structure models for calculating synthetic waveforms, and maximum amplitudes of the observed (red) and synthetic (black) waveforms are shown to the left of each waveformBack to article page