COMPOSITION AND MORPHOLOGY OF SEAFLOOR HIGHS IN THE SOUTHWESTERN GREENLAND CONTINENTAL MARGIN

Ovsyannikov A.O.; Bobrov A.V.

dc.contributor.author	Ovsyannikov A.O.
dc.contributor.author	Bobrov A.V.
dc.date.accessioned	2024-11-09T08:38:19Z
dc.date.available	2024-11-09T08:38:19Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13528518
dc.identifier.citation	Geochemistry International, 2006, 44, 6, 613-618
dc.identifier.issn	0016-7029
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46439
dc.description.abstract	The Greenland continental margin is a modern example of a passive margin formed as a result of the opening of the northern Atlantic in the Late Mesozoic–Early Cenozoic. The time of the beginning of spreading in the Labrador Sea is not precisely known. There were attempts to reconstruct seafloor spreading history, by the identification and calculation of magnetic anomalies in the Labrador Sea. It is supposed that the opening of the oceanic basin started 68 Ma ago.
dc.title	COMPOSITION AND MORPHOLOGY OF SEAFLOOR HIGHS IN THE SOUTHWESTERN GREENLAND CONTINENTAL MARGIN
dc.type	Статья
dc.identifier.doi	10.1134/S0016702906060061