ON TWO TYPES OF METALLIFEROUS CARBONACEOUS ROCKS

dc.contributor.author	Tomson I.N.
dc.contributor.author	Polyakova O.P.
dc.contributor.author	Alekseev V.Yu.
dc.contributor.author	Baskina V.A.
dc.date.accessioned	2024-12-15T02:15:15Z
dc.date.available	2024-12-15T02:15:15Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13505919
dc.identifier.citation	Geology of Ore Deposits, 2006, 48, 1, 74-76
dc.identifier.issn	1075-7015
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46979
dc.description.abstract	Two types of metalliferous carbonaceous rocks that differ in associated metals are considered. One of them is characterized by gold occurring in finely dispersed arsenopyrite and arsenic-bearing pyrite, and the other, by finely impregnated native metals in carbonaceous matter. Rocks of the first type also contain elements of the platinum group, while those of the second type bear rhenium, silver, iron, molybdenum, and other metals. Graphitic mineralization is usually localized in the shear zone associated with alkaline basalts. © Pleiades Publishing, Inc., 2006.
dc.title	ON TWO TYPES OF METALLIFEROUS CARBONACEOUS ROCKS
dc.type	Статья
dc.identifier.doi	10.1134/S1075701506010053

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