PRECIOUS METAL MINERALIZATION IN LOW-SULFIDE ORES OF THE IOKO-DOVYREN LAYERED MASSIF, NORTHERN BAIKAL REGION

dc.contributor.author	Orsoev D.A.
dc.contributor.author	Rudashevsky N.S.
dc.contributor.author	Kretser Yu.L.
dc.contributor.author	Konnikov E.G.
dc.date.accessioned	2022-01-16T05:05:34Z
dc.date.available	2022-01-16T05:05:34Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=13444728
dc.identifier.citation	Doklady Earth Sciences, 2003, 390, 4, 545-549
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/34360
dc.description.abstract	The largest ore deposits of platinum group metals are assigned to the low-sulfide type. They are commonly confined to specific units (reefs) within large layered massifs (Bushveld, Stillwater, Great Dike, Fedorov-Panskii, Penikat, and others). Rocks of these units are characterized by maximal petrographic and mineralogical heterogeneity. Ore mineralization therein is characterized by a very low content of sulfide minerals, high concentrations of platinum group elements (PGEs), and an abundance of minerals with volatile components. The Pt-bearing unit recently revealed in the Ioko-Dovyren layered massif is a prominent example [1-4].
dc.title	PRECIOUS METAL MINERALIZATION IN LOW-SULFIDE ORES OF THE IOKO-DOVYREN LAYERED MASSIF, NORTHERN BAIKAL REGION
dc.type	Статья

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