Fig. 12From: Surface wave group velocity in the Osaka sedimentary basin, Japan, estimated using ambient noise cross-correlation functionsComparison among Love and Rayleigh wave group velocities (open circles) estimated from tomography analysis and the theoretical dispersion curves from the UMC2013 model (red line) and Iwata et al. (2008) model (blue line) at cells (I x , I y ) = (2, 5), (5, 6), and (8, 4), where I x and I y are the number of cells in the X and Y directions, respectively, as shown on the map. The S-wave velocity profiles corresponding to theoretical dispersion curves are shown in the right column Back to article page