Fig. 7From: Ambient noise tomography for a high-resolution 3D S-wave velocity model of the Kinki Region, Southwestern Japan, using dense seismic array dataHorizontal slices of the S-wave velocity model at discrete depth levels below sea level. Depth is shown above each respective panel. a–f S-wave velocity models without showing the active faults (S-wave velocity models before correcting for the effects of topography are shown in Figure S4). NM and KM represent the prominent high-velocity anomaliesBack to article page