A NEW TYPE OF NOBLE METAL MINERALIZATION IN TERRIGENOUS ROCKS OF THE SHATAK GRABEN, WESTERN SLOPE OF THE SOUTHERN URALS

Kovalev S.G.; Vysotskii I.V.

dc.contributor.author	Kovalev S.G.
dc.contributor.author	Vysotskii I.V.
dc.date.accessioned	2024-12-22T03:47:44Z
dc.date.available	2024-12-22T03:47:44Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13531837
dc.identifier.citation	Lithology and Mineral Resources, 2006, 41, 4, 371-377
dc.identifier.issn	0024-4902
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/47031
dc.description.abstract	The paper presents materials on a new (unconventional for the Urals) noble metal (platinum-gold-iron oxide) mineralization confined to terrigenous sequences of the Middle Riphean Mashak Formation on the western slope of the southern Urals. The mineralization is related to the percolation of reduced mantle fluids into upper levels of the crust at early stages of riftogenesis, their inversion in the crust, and redeposition of oreforming elements. © Pleiades Publishing, Inc. 2006.
dc.subject	Riphean
dc.title	A NEW TYPE OF NOBLE METAL MINERALIZATION IN TERRIGENOUS ROCKS OF THE SHATAK GRABEN, WESTERN SLOPE OF THE SOUTHERN URALS
dc.type	Статья
dc.identifier.doi	10.1134/S0024490206040079
dc.subject.age	Precambrian::Proterozoic::Riphean
dc.subject.age	Докембрий::Протерозой::Рифей