Fig. 3From: Difference of horizontal-to-vertical spectral ratios of observed earthquakes and microtremors and its application to S-wave velocity inversion based on the diffuse field conceptMeasured EHVR at a measurement point EHM012. The averaged EHVR (red), average ± one standard deviation (orange), and individual EHVRs (black). Left: S-wave part, right: coda part immediately after S-wave partBack to article page