1887

Abstract

In accordance with experimental data, in many cases sedimentary deposits are found to be anisotropic media for long seismic waves. With sufficient approximation the model of these rocks is transversely isotropic media (TIM) with horizontal or vertical plane of isotropy, and they are called polar or azimuthal anisotropy, respectively.

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/content/papers/10.3997/2214-4609.201411017
1991-05-28
2020-04-03
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201411017
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