Fig. 5From: Estimation of the source process and forward simulation of long-period ground motion of the 2018 Hokkaido Eastern Iburi, Japan, earthquakeSimulated PGV distribution. The PGV is the maximum absolute amplitude of the vector sum of the three-component velocity waveforms low-pass filtered at 0.5 Hz. The triangles denote the observed PGV at K-NET and KiK-net stations for comparisonBack to article page