CARBONATITE SOURCES OF THE II'MENY-VISHNEVOGORSK COMPLEX: EVIDENCE FROM SR AND ND ISOTOPE DATA ON CARBONATES

dc.contributor.author	Pribavkin S.V.
dc.contributor.author	Nedosekova I.L.
dc.date.accessioned	2024-10-27T02:28:51Z
dc.date.available	2024-10-27T02:28:51Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13514448
dc.identifier.citation	Doklady Earth Sciences, 2006, 408, 4, 627-630
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46281
dc.description.abstract	The alkaline–carbonatite complex of the Paleozoic structure of the Urals is located in the Precambrian Sysert–Il’menogorsk block, which includes two structural levels and experienced a long-term evolution. The core of the block (lower structural level) is composed of the diaphthoritic gneiss granulites and migmatites of the Selyanka Sequence with the U–Pb zircon age of 1820 ± 70 Ma.
dc.title	CARBONATITE SOURCES OF THE II'MENY-VISHNEVOGORSK COMPLEX: EVIDENCE FROM SR AND ND ISOTOPE DATA ON CARBONATES
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X0604026X

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