Fig. 13From: Investigation of the subsurface structure at the target site in Kumamoto, Japan, and the distributed data of the blind prediction exercise: report for the experiments for the 6th international symposium on effects of surface geology on seismic motionObserved spectral ratios between KUMA and KU.KMP1 (gray line) compared with calculated amplification from layers of Vs = 1100 m/s, Vs = 2100 m/s and Vs = 3200 m/s in red, blue and green lines, respectively, to the surface of the preferred velocity modelBack to article page