NEOTECTONICS OF THE NORTHERN NORWEGIAN-GREENLAND BASIN: SPECIFIC FEATURES AND EVOLUTION OF THE KNIPOVICH RIDGE AND POMORSKY PERIOCEANIC TROUGH

dc.contributor.author	Shipilov E.V.
dc.contributor.author	Shkarubo S.I.
dc.contributor.author	Raznitsin Yu.N.
dc.date.accessioned	2024-10-23T07:15:46Z
dc.date.available	2024-10-23T07:15:46Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13509041
dc.identifier.citation	Doklady Earth Sciences, 2006, 410, 7, 1056-1061
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46114
dc.description.abstract	The Earth’s crust beneath the Atlantic Ocean has a heterogeneous tectonic structure. The northern (Arctic and subarctic) region is characterized by a particularly specific structure. The region is located between two demarcation fracture zones. The Spitsbergen fracture zone, which separates the study region from structures of the Polar Basin, is situated in the north. The Charley Gibbs fracture zone (52° N) is located in the south. The Reykjanes spreading ridge, which extends from Iceland to the southwest, is obviously a member of the Mid-Atlantic Ridge system.
dc.title	NEOTECTONICS OF THE NORTHERN NORWEGIAN-GREENLAND BASIN: SPECIFIC FEATURES AND EVOLUTION OF THE KNIPOVICH RIDGE AND POMORSKY PERIOCEANIC TROUGH
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06070129

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