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Abstract

The Barents Sea still contains a number of exciting new plays and prospects. The Western Nordkapp Basin is a little explored basin located in the easternmost portion of the Norwegian Barents Sea. The basin is essentially a deep Paleozoic and Triassic depocenter punctuated by salt walls which strike parallel to the basin axis. Structuring associated with these diapirs has created a number of interesting plays which are currently being evaluated in the Norwegian Fourteenth Licensing Round.

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/content/papers/10.3997/2214-4609.201411748
1993-06-08
2024-04-17
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201411748
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