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Abstract

Astrong impedance contrast, such as the base of the Cretaceous in the North Sea, generates a train of high amplitude water bottom peg legs which can heavily obscure the underlying less energetic reflections, often of great petroleum interest. Attenuation of these peg legs, a prerequisite for defining the structural image, is a persistent and difficult problem in processing the seismic data.

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/content/papers/10.3997/2214-4609.201410776
1991-05-28
2024-04-19
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410776
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