1887

Abstract

Herein, we expand and use the method used by Landa and Keydar (1998) to detect local heterogeneities. The method relies on computing local semblance along the diffraction offset-traveltime curves. We expand the method by taking into account the phase change occurring for edge diffractions. We demonstrate the usefulness of the method on hard-rock seismic data.

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/content/papers/10.3997/2214-4609.20130702
2013-06-10
2024-04-24
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20130702
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