A NEW TYPE OF ORE MINERALIZATION IN PRECAMBRIAN CONGLOMERATES ON THE WESTERN SLOPE OF THE SOUTHERN URALS

dc.contributor.author	Kovalev S.G.
dc.contributor.author	Vysotskii I.V.
dc.date.accessioned	2022-08-14T03:31:09Z
dc.date.available	2022-08-14T03:31:09Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13471405
dc.identifier.citation	Doklady Earth Sciences, 2004, 395, 3, 331-334
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38532
dc.description.abstract	Precambrian conglomerates are known in composition of Marshakskaya suite (R2) within the western slope of the Southern Ural. Terrigenic and other formations are noted in the paleoriftogenic structure. Investigations of the terrigenic formations have been performed. Results of the investigations have made it possible to obtain original information on their metal-bearing behavior. New type of noble-metal mineralization for Ural has been separated. Geological information and the investigation results show that complex platinum-gold-iron oxide mineralization is new one for Ural.
dc.subject	Precambrian
dc.title	A NEW TYPE OF ORE MINERALIZATION IN PRECAMBRIAN CONGLOMERATES ON THE WESTERN SLOPE OF THE SOUTHERN URALS
dc.type	Статья
dc.subject.age	Precambrian
dc.subject.age	Докембрий	ru

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