Fig. 11From: Source rupture process of the 2018 Hokkaido Eastern Iburi earthquake deduced from strong-motion data considering seismic wave propagation in three-dimensional velocity structureMaps showing comparison between the simulated PGV (background color) and observed PGV (colored circles). Both of the simulated and observed waveforms were low-pass filtered at 0.5 Hz. The star indicates the epicenterBack to article page