Fig. 13From: Cause of destructive strong ground motion within 1–2 s in Mukawa town during the 2018 Mw 6.6 Hokkaido eastern Iburi earthquakeTheoretical site amplification factor of the SH-wave for three sites. The theoretical site amplification factor calculated with the estimated Vs structures in Fig. 9 and Table 2. The SH-wave was assumed to input for 1.3 km/s layer with an incident angle of 0°Back to article page