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Abstract

The traditional approach to studying seismic anisotropy is based on using elastic parameters Cij according to generalised Hook's law. The geological medium is approximated by a homogeneous anisotropic model in which seismic rays are straight lines.

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/content/papers/10.3997/2214-4609.201411006
1991-05-28
2024-04-25
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201411006
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