Fig. 6From: High-resolution three-dimensional azimuthal velocity anisotropy of S-waves in southern-central Japan, based on ambient noise tomographya–f Horizontal slices showing the variation of isotropic S-wave velocities (background color) and azimuthal anisotropy (black bars) at discrete depth levels below sea level. White lines show the location of documented active faults. Depth (in km) is shown above each respective panel. Also shown is the location of the Median Tectonic Line (MTL) and sedimentary basins (black, dashed closed curves in b)Back to article page