1887

Abstract

In the present structural pattern of the West Arctic Offshore three deep sedimentary basins filled with thick Upper Paleozoic, Mesozoic and Cenozoic, predominantly, terrigenous sediments are differentiated: - Barerts Sea Basin - South Kara Basin - Laptev Sea Basin

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/content/papers/10.3997/2214-4609.201409606
1995-05-29
2020-06-05
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409606
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