Fig. 9From: Lithosphere–asthenosphere boundary beneath the Sea of Japan from transdimensional inversion of S-receiver functionsRadial-component responses of a sediment layer overriding a half space. a Algebraic expression given by Equation \(18\). Color notation is the same as Fig. 8a. b Numerical results. The velocity model shown by the red line in Fig. 8a is used. The incident plane S-wave has a ray parameter of 0.11 s/km and a unit amplitudeBack to article page