EVOLUTION OF THE RIFT ZONE MORPHOSTRUCTURE IN THE NORTH ATLANTIC MAGMATIC PROVINCE

dc.contributor.author	Il'in A.V.
dc.date.accessioned	2024-10-27T02:28:50Z
dc.date.available	2024-10-27T02:28:50Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13518447
dc.identifier.citation	Doklady Earth Sciences, 2006, 411, 9, 1497-1500
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46276
dc.description.abstract	The North Atlantic region, which is located between the Charlie Gibbs Fracture Zone in the south and the Nansen Ridge in the north, has long been known as the Tule volcanic province coined after the ancient name of Iceland Island holding a central position in the province. Tule Province, ~3500 km long, was the last fragment of the continental crust in the Atlantic Ocean. In the Tertiary, the whole region underwent intense tectonomagmatic activity.
dc.title	EVOLUTION OF THE RIFT ZONE MORPHOSTRUCTURE IN THE NORTH ATLANTIC MAGMATIC PROVINCE
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06090376

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