Diffraction of a Plane Elastic Wave by a Gradient Transversely Isotropic Layer
Figure 5
Dependence of normalized energy of the transmitted longitudinal wave having the angular frequency rad/sec on its angle of incidence upon a siltstone layer of thickness L = 10 m placed into sandstone. The solid curve corresponds to a uniform layer of siltstone, the dotted curve “compressed siltstone,” and the dashed curve “relaxed siltstone.”
