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Fig. 9 | Earth, Planets and Space

Fig. 9

From: Subsurface structure identification at the blind prediction site of ESG6 based on the earthquake-to-microtremor ratio method and diffuse field concept for earthquakes

Fig. 9

Comparison of the estimated HSAF at the nearest (~ 1.2 km away) JMA station, EEB by GIT (Nakano et al., 2015), with the theoretical one-dimensional HSAFs by the inverted S-wave velocity profiles from EHVR and pEHVR, together with the HSAF by the preferred model. A geological map by Geological Survey of Japan (https://gbank.gsj.jp/seamless/) on the top shows the location of EEB relative to KUMA. The constant damping ratio of 1.1% is assumed for the pEHVR profile and preferred model, while the Vs-dependent damping (Table 3) is assumed for the EHVR profile

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