1887

Abstract

We consider a modification of duplex wave migration that enables seismic images of subvertical boundaries formed by waves of fixed incident angles to be obtained. This allows us to conduct AVO analysis of the subvertical boundaries for classification of faults and estimation of their properties. The role of a full-wave modeling for corrections required to obtain undistorted AVO curves is demonstrated.

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/content/papers/10.3997/2214-4609.20145609
2010-05-04
2024-03-29
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20145609
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