Fig. 5From: Ambient noise tomography for a high-resolution 3D S-wave velocity model of the Kinki Region, Southwestern Japan, using dense seismic array dataRay paths derived from the inversion model at two selected frequencies: a 0.5Â Hz and b 0.2Â Hz. Also shown are the locations of permanent seismic stations (black triangles) and temporary seismic stations (red triangles). Blue lines indicate ray pathsBack to article page