Seismic waves in a stratified half space.

摘要: Summary. The response of a stratified elastic half space to general source may be represented in terms the reflection and transmission properties regions above below source. For P-SV SH waves both buried sources receivers, convenient forms found which no loss precision problems arise from growing exponential evanescent regime. These expressions have ready physical interpretation enable useful approximations developed. representation leads efficient computational procedures for models composed uniform layers, extended an asymptotic development piecewise smooth models.