Fig. 10From: Long-period ground motion simulation using centroid moment tensor inversion solutions based on the regional three-dimensional model in the Kanto region, JapanComparisons between observed and simulated seismograms for periods of 15–30 s. We selected two F-net (N.ASIF and N.JIZF) and three MeSO-net (E.YYIM, OK.KTGM, and E.YROM) stations. Amplitudes at each station were normalized by the maximum amplitudes of observed seismograms for periods of 15–30 s at each station. a Event A, b Event B, and c Event C. Gray and blue dotted lines are the observed and simulated seismograms, respectively. Left panels show used stations and bedrock depths of the JIVSM. Color for bedrock depths is similar as Fig. 1Back to article page