Synthetic seismograms. The solution is decomposed into generalized rays, and the effects of attenuation and dispersion are incorporated in an ad hoc manner in the frequency domain. The results are illustrated with synthetics for a model simulating a weathered layer over a half-space. Both the SH and P-SV cases are treated.--Modified journal abstract.

This content is PDF only. Please click on the PDF icon to access.

First Page Preview

First page PDF preview
You do not currently have access to this article.