1887

Abstract

Seismic interpretation in principal tries to find any small changes, as subtle stratigraphic plays and areas of low-relief faulting. Looking at the amplitude of reflections at particular frequencies may be helpful to see more clearly features which may no

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/content/papers/10.3997/2214-4609.201400203
2009-06-08
2024-04-19
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400203
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