EVOLUTION OF THE SOUTHERN PART OF THE CANADA BASIN (ARCTIC OCEAN) BASED ON MAGNETOMETRIC DATA

dc.contributor.author	Gurevich N.I.
dc.contributor.author	Merkur'ev S.A.
dc.contributor.author	Abel'skaya A.A.
dc.date.accessioned	2024-10-27T02:28:43Z
dc.date.available	2024-10-27T02:28:43Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13516248
dc.identifier.citation	Doklady Earth Sciences, 2006, 407, 2, 308-311
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46243
dc.description.abstract	Using a new Russian–American digital grid of anomalous magnetic field of the Arctic Ocean, oceanic magnetic anomalies were identified for the whole southern part of the Canada Basin (hereafter, southern CB), extending from the eastern scarp of the Northwind Ridge to the adjacent Banks Island–Mackenzie Delta continental margin. The geohistorical analysis of magnetic anomalies carried out based on the original procedure revealed regional features of the basin evolution. Contradictory ideas about this evolution were so far based on the geology of continental framing.
dc.title	EVOLUTION OF THE SOUTHERN PART OF THE CANADA BASIN (ARCTIC OCEAN) BASED ON MAGNETOMETRIC DATA
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06020358

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