THE OLDEST GRANITOIDS IN THE TRANSANGARA REGION OF THE YENISEI RIDGE: U-TH-PB DATA ON ZIRCON

dc.contributor.author	Vernikovskaya A.E.
dc.contributor.author	Vernikovsky V.A.
dc.contributor.author	Popov N.V.
dc.contributor.author	Yasenev A.M.
dc.contributor.author	Wingate M.T.D.
dc.date.accessioned	2022-07-20T06:12:20Z
dc.date.available	2022-07-20T06:12:20Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13458237
dc.identifier.citation	Doklady Earth Sciences, 2004, 397, 5, 616-620
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38312
dc.description.abstract	It is established that in Transangara distinctly specified is the most early Neoproterozoic collision event in the range of 865-880 mln years ago. According to the determined geologic position, chemical composition and granitoids formation age, the integral Teiskii complex includes, apart from the considered Teiskii and Kalaminskii massifs, granites of Erudinskii massif with the age 878 mln years. Most likely, the granites of this complex were formed outside Siberian shield, being within Central-Angara terrein already before its collision with Siberia.
dc.title	THE OLDEST GRANITOIDS IN THE TRANSANGARA REGION OF THE YENISEI RIDGE: U-TH-PB DATA ON ZIRCON
dc.type	Статья

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