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MOESM2 of Source rupture process of the 2018 Hokkaido Eastern Iburi earthquake deduced from strong-motion data considering seismic wave propagation in three-dimensional velocity structure

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posted on 2019-09-19, 04:10 authored by Kimiyuki Asano, Tomotaka Iwata
Additional file 2: Fig. S2. Comparison of the observed velocity waveforms (black traces) and the synthetic velocity waveforms using JIVSM (red traces) in 0.04–0.5 Hz for the MW 4.1 aftershock at 09:48 on September 14, 2018. 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–down.

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