Fig. 11From: Lithosphere–asthenosphere boundary beneath the Sea of Japan from transdimensional inversion of S-receiver functionsComparison to surface wave tomography model. a Seafloor topography profile. b Cross section of S-wave velocity model estimated by surface wave tomography (Yoshizawa et al. 2010). The shallow portion (< 30 km depth) is masked by the gray shade because of insufficient resolution with long-period surface waves. Blue horizons roughly indicate the lithosphere–asthenosphere boundary inferred from the inversion. Red squares denote station locations. c Profile location (red line) and station locations (red squares)Back to article page