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Abstract

In this paper we study the influence of porosity fluctuations and fluid properties on the propagation of obliquely incident P-,SV- and SH- seismic plane waves in a poroelastic, fluid-saturated, and finely layered medium.

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/content/papers/10.3997/2214-4609.201409446
1995-05-29
2021-06-16

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