The system of ODE that governs elastic-wave propagation in plane stratified media becomes singular as the elastic rigidity approaches zero. Two approximate methods are presented to address the problem. First, for P-SV waves, one can impose the condition that the displacement is curl-free in the transitional solid. This condition suppresses shear waves. Second, one can represent a thin transitional solid as a massive elastic interface (MEI). The MEI boundary conditions do not become singular as the MEI rigidity approaches zero.
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CITATION STYLE
Gilbert, F. (1998). Elastic waves in a transitional solid with arbitrarily small rigidity. Geophysical Journal International, 133(2), 230–232. https://doi.org/10.1046/j.1365-246X.1998.00486.x