NEW SHRIMP U-PB AGE DATA ON ZIRCONS FROM PLAGIOGRANITES IN THE OPHIOLITES OF THE KAMCHATSKY MYS PENINSULA, EASTERN KAMCHATKA

dc.contributor.author	Luchitskaya M.V.
dc.contributor.author	Tsukanov N.V.
dc.contributor.author	Skolotnev S.G.
dc.date.accessioned	2024-10-19T07:54:52Z
dc.date.available	2024-10-19T07:54:52Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13507210
dc.identifier.citation	Doklady Earth Sciences, 2006, 408, 4, 535-537
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46089
dc.description.abstract	Three ophiolite complexes of different ages and paleotectonic settings were recognized at the Kamchatsky Mys Peninsula, eastern Kamchatka. Their age was determined from geological data and the microfaunal assemblage of the upper siliceous sediments associated with volcanic rocks. SHRIMP U–Pb zircon dating was conducted for plagiogranites to confirm the geological age of the ophiolites. The plagiogranites pertain to the Upper Cretaceous ophiolite complex, which consists of depleted peridotites, gabbroids cut by dikelike plagiogranite bodies, island-arc tholeiites, and boninites.
dc.title	NEW SHRIMP U-PB AGE DATA ON ZIRCONS FROM PLAGIOGRANITES IN THE OPHIOLITES OF THE KAMCHATSKY MYS PENINSULA, EASTERN KAMCHATKA
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06040064
dc.subject.age	Мезозой::Меловая

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