1887

Abstract

Seismic profiles shot in Barents Sea cross a number of potential reef features, located between two reliable reflections at the top of Paleozoic and within the Paleozoic, 200 ms deeper. Conventional seismic work using P-waves is unable to separate porous from dry reefs, and all the more to assess the fluid contents.

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/content/papers/10.3997/2214-4609.201411396
1993-06-08
2020-04-04
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201411396
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