PALEOGEOGRAPHIC SETTINGS AND TECTONIC DEFORMATIONS OF THE BARENTS SEA CONTINENTAL MARGIN IN THE CENOZOIC

Shipilov E.V.; Golubev V.A.; Tyuremnov V.A.; Glaznev V.N.

dc.contributor.author	Shipilov E.V.
dc.contributor.author	Golubev V.A.
dc.contributor.author	Tyuremnov V.A.
dc.contributor.author	Glaznev V.N.
dc.date.accessioned	2024-11-09T08:38:08Z
dc.date.available	2024-11-09T08:38:08Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13526125
dc.identifier.citation	Doklady Earth Sciences, 2006, 407, 3, 366-371
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46404
dc.description.abstract	The Barents Sea continental margin (hereafter, Barents margin) differs from other passive margins by the most extensive shelf, the giant thickness of sedimentary rocks in basins and troughs, and its unique tectonic position. The outer, almost rectangular promontory of the Barents margin juts out into its deepwater western and northern framing, identified as the Norwegian–Greenland and Eurasia basins, respectively. In this regard, the continental margin is affected by two, mutually perpendicular spreading zones (Knipovich and Gakkel ridges).
dc.subject	PALEOGEOGRAPHIC SETTINGS
dc.subject	TECTONIC DEFORMATIONS
dc.subject	BARENTS SEA
dc.subject	CONTINENTAL MARGIN
dc.title	PALEOGEOGRAPHIC SETTINGS AND TECTONIC DEFORMATIONS OF THE BARENTS SEA CONTINENTAL MARGIN IN THE CENOZOIC
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06030056