Fig. 11From: Kinematic source models for long-period ground motion simulations of megathrust earthquakes: validation against ground motion data for the 2003 Tokachi-oki earthquakeDistribution of 5 % damped velocity response spectra (Sv). a Model 0, b Model C, and c Model H3 averaged over 25 heterogeneous patterns at periods of 2, 3, 5, 7, and 10 s. Observed Sv at K-NET and KiK-net stations are plotted with small circles. Gray rectangles indicate the configurations of the fault and the asperitiesBack to article page