1887

Abstract

There exist some remarkable, shallow anomalies above the Eocene Frigg Gamma structure in the northern North Sea. The anomalies formed as a result of huge hydrocarbon leakage from the Frigg Gamma structure. Biodegradation processes resulted in extensive calcite cementation that occurs in a zone of more than 400 m in the Miocene sandy section.

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/content/papers/10.3997/2214-4609.20147432
2014-11-23
2024-04-20
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20147432
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