Fig. 10From: Source rupture process of the 2018 Hokkaido Eastern Iburi earthquake deduced from strong-motion data considering seismic wave propagation in three-dimensional velocity structurePasted up of the simulated seismic velocity waveforms along the profile E–E′. The location of the profile line is shown in Fig. 11. a EW, b NS component. The origin (0 km) of the horizontal axis corresponds to the location of the epicenter, which was indicated by the star in Fig. 11Back to article page