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Abstract

The main difficulty in extending seismic processing to anisotropic media is the recovery of anisotropic velocity fields from surface reflection data. As shown by Tsvankin and Thomsen (1995), P-wave moveout from horizontal reflectors is insufficient to obtain the parameters of transversely isotropic media with a vertical symmetry axis (VTI), even if long spreads (twice the reflector depth) are used.

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/content/papers/10.3997/2214-4609.201409400
1995-05-29
2022-05-28
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409400
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