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Center for Lithospheric Studies The University of Texas at Dallas, P.O. Box 830688, MS FA31, Richardson, Texas 75083-0688
Abstract
An extension of the boundary integral method for SH waves is given for transversely isotropic media. The accuracy of the method is demonstrated for a simple flat interface problem by comparison to the Cagniard-de Hoop solution. The method is further demonstrated for a case with interface topography for both surface and vertical seismic profiles. The new method is found to be both accurate and effective.
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