Fig. 6From: Source rupture process of the 2018 Hokkaido Eastern Iburi earthquake deduced from strong-motion data considering seismic wave propagation in three-dimensional velocity structureComparison of the observed velocity waveforms (black traces) and the synthetic velocity waveforms (red traces) in 0.04–0.5 Hz. The amplitudes were normalized by the maximum observed amplitude. The maximum observed amplitude of each component is shown above each trace in units of cm/s. NS north–south, EW east–west, UD up–downBack to article page