1887

Abstract

The effect of waves attenuation because of scattering in layered media can be observed and analyzed in data of seismic measurements like VSP and cross-hole sounding. Theoretically and numerically we consider the transmission of a pressure plane wave through an extensive fragment of a stratified disordered medium with constant density and without intrinsic attenuation. We study effects of multiple scattering.

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/content/papers/10.3997/2214-4609.201410422
1992-06-01
2020-11-25
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410422
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