1887

Abstract

The variation of the amplitudes of seismic reflection data as a function of angle of incidence or offset (AVO) is a<br>technique that is widely applied in exploration for hydrocarbons and the characterization of reservoirs. Many<br>approximations of the Zoeppritz equations have been proposed, and another one is added here to add to the general<br>confusion. A simple method of comparing them is used here to compare two approximations with the full solution.

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/content/papers/10.3997/2214-4609-pdb.154.021
2005-09-14
2020-01-22
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.154.021
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