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

dc.contributor.authorLuchitskaya M.V.
dc.contributor.authorTsukanov N.V.
dc.contributor.authorSkolotnev S.G.
dc.date.accessioned2024-10-19T07:54:52Z
dc.date.available2024-10-19T07:54:52Z
dc.date.issued2006
dc.description.abstractThree 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.identifierhttps://www.elibrary.ru/item.asp?id=13507210
dc.identifier.citationDoklady Earth Sciences, 2006, 408, 4, 535-537
dc.identifier.doi10.1134/S1028334X06040064
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/46089
dc.subject.ageМезозой::Меловая
dc.titleNEW SHRIMP U-PB AGE DATA ON ZIRCONS FROM PLAGIOGRANITES IN THE OPHIOLITES OF THE KAMCHATSKY MYS PENINSULA, EASTERN KAMCHATKA
dc.typeСтатья

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