Fig. 3From: Subsurface structure identification at the blind prediction site of ESG6 based on the earthquake-to-microtremor ratio method and diffuse field concept for earthquakesComparisons of the theoretical EHVRs by the inverted models with the observed EHVR on the left and the resultant S-wave and P-wave velocity profiles on the right. Light gray lines are the results of ten trials and the black lines are the best among them. Orange lines are those of the JIVSM structure close to KUMA (Koketsu et al. 2012). The inclined dashed and dotted lines on velocity models show resonant frequencies of the corresponding layer interfaces based on one quarter wavelength lawBack to article page