U-PB (SHRIMP II) AGE OF ZIRCONS FROM ASH BEDS OF THE CHERNOKAMEN FORMATION, VENDIAN SYLVITSA GROUP (CENTRAL URALS)

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dc.contributor.author Ronkin Yu.L.
dc.contributor.author Maslov A.V.
dc.contributor.author Mizens G.A.
dc.contributor.author Krupenin M.T.
dc.contributor.author Petrov G.A.
dc.contributor.author Lepikhina O.P.
dc.contributor.author Kornilova A.Yu.
dc.contributor.author Grazhdankin D.V.
dc.contributor.author Matukov D.I.
dc.date.accessioned 2024-10-27T02:28:49Z
dc.date.available 2024-10-27T02:28:49Z
dc.date.issued 2006
dc.identifier https://www.elibrary.ru/item.asp?id=13518443
dc.identifier.citation Doklady Earth Sciences, 2006, 411, 9, 1341-1345
dc.identifier.issn 1028-334X
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/46272
dc.description.abstract The Serebryanka and Sylvitsa groups on the western slope of the Urals characterize the Vendian section of the eastern folded framework of the East European Platform [1]. They are conspicuous against the background of the coeval platformal sequences by their relatively complete sedimentary record, sufficiently good outcrops, and opportunities for detailed sedimentological study both along and across the regional paleoslope. The tillite units serve as key elements of the stratigraphic framework of the Serebryanka Group.
dc.subject Serebryanka
dc.subject Sylvitsa
dc.subject Urals
dc.subject Vendian
dc.title U-PB (SHRIMP II) AGE OF ZIRCONS FROM ASH BEDS OF THE CHERNOKAMEN FORMATION, VENDIAN SYLVITSA GROUP (CENTRAL URALS)
dc.type Статья
dc.identifier.doi 10.1134/S1028334X06090029
dc.subject.age Precambrian::Proterozoic::Neoproterozoic::Vendian
dc.subject.age Докембрий::Протерозой::Неопротерозойская::Вендский


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