PLATINUM-PALLADIUM MINERALIZATION IN CHROMITE ORES FROM ULTRABASIC ROCKS OF THE WESTERN SAYAN REGION

dc.contributor.author	Podlipsky M.Yu.
dc.contributor.author	Krivenko A.P.
dc.contributor.author	Polyakov G.V.
dc.date.accessioned	2022-07-20T06:12:18Z
dc.date.available	2022-07-20T06:12:18Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13456443
dc.identifier.citation	Doklady Earth Sciences, 2004, 396, 4, 508-511
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38285
dc.description.abstract	The Kalna Massif incorporates a specific PGM mineral assemblage. Data on analogous ophiolite complexes in other regions of the world [3] suggest a comercial significance of the Kalna PGM mineralization characterized by the prevalence of Pd-rich Pt-Fe-Cu alloys, diversity of mineral phases. and multistage character of evolution. The late hydrothermal stages of the Kalna Massif include Pd- and Rh-rich minerals that are atypical of alpine-type ultrabasic rocks. The discovered Pt-chromite mineralization can be considered a new and important source of PGMs in Russia.
dc.title	PLATINUM-PALLADIUM MINERALIZATION IN CHROMITE ORES FROM ULTRABASIC ROCKS OF THE WESTERN SAYAN REGION
dc.type	Статья

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