1887

Abstract

In this paper the EEI (extended elastic impedance) projection technique is used to discriminate lithologies from a land wide azimuth survey. AVO intercept / gradient data are inverted to the impedance domain followed by cross-plotting the extracted seismi

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/content/papers/10.3997/2214-4609.201400016
2009-06-08
2024-03-29
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400016
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