ZIRCONS AND THE PROBLEM OF PRECAMBRIAN IN THE MAIN GRANITE BELT OF THE URALS: EVIDENCE FROM THE KOZHUBAEVO METAMORPHIC COMPLEX

dc.contributor.author	Krasnobaev A.A.
dc.contributor.author	Fershtater G.B.
dc.contributor.author	Bea F.
dc.contributor.author	Montero P.
dc.date.accessioned	2024-10-23T07:16:02Z
dc.date.available	2024-10-23T07:16:02Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13512597
dc.identifier.citation	Doklady Earth Sciences, 2006, 408, 4, 612-616
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46164
dc.description.abstract	Metamorphic rocks of the Kozhubaevo Complex (KC) surround the Dzhabyk–Karagai granite massif in the north and northwest. Together with granites, the metamorphic rocks belong to the Ural–Tobol’sk anticlinorium of the East Uralian Anticlinorium. The issue of the KC age is a characteristic problem of all similar gneissic complexes in the Urals, since geological data suggest both Paleozoic and Precambrian ages for the gneisses, while geochronological data are limited by only a few K–Ar datings within 250–350 Ma.
dc.subject	Kozhubaevo Complex
dc.subject	Urals
dc.subject	Cambrian
dc.title	ZIRCONS AND THE PROBLEM OF PRECAMBRIAN IN THE MAIN GRANITE BELT OF THE URALS: EVIDENCE FROM THE KOZHUBAEVO METAMORPHIC COMPLEX
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06040234
dc.subject.age	Paleozoic::Cambrian
dc.subject.age	Палеозой::Кембрийская

Files in this item

Name: Kras_06.pdf

Size: 255.4Kb

Format: PDF