1887

Abstract

Recent seismic surveys and reprocessing by Sevoteam/MAGE make it possible to verify and add information about the sedimentary cover especially Lower Paleozoic terrigenous and carbonate complex (Cambrian-Lower Permian) within the southern part of the Barents Shelf, including the aquatorial continuation of the Pechora Platform, Kola-Kaniri Monocline, South Barents Basin, West-Kola Saddle and other structures.

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/content/papers/10.3997/2214-4609.201409684
1995-05-29
2020-09-25
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409684
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