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Abstract

The seismic velocity can be used to separate primary and multiple reflections for prediction of reservoir porosities and rock lithology, as well as for construction of depth maps.

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/content/papers/10.3997/2214-4609.201409488
1995-05-29
2024-04-19
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409488
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