MASSIVE SULFIDE ORES OF THE URALS: A NEW GENERAL MINERALOGICAL OBJECT

dc.contributor.author	Chesnokov B.V.
dc.contributor.author	Zaikov V.V.
dc.contributor.author	Melekestseva I.Yu.
dc.date.accessioned	2022-01-14T04:15:14Z
dc.date.available	2022-01-14T04:15:14Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=13435962
dc.identifier.citation	Doklady Earth Sciences, 2003, 393, 9, 1336-1337
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/34292
dc.description.abstract	The main pyrite deposits in Ural region are concentrated in Tagilskaya and Magnitogorskaya metallogenic zones formed in middle Paleozoic period. These structures have length of 1,500 km and width of several tens km. They are characterized by the leading positions in respect with reserves of Co plus Pb plus Zn (55 million tons). About 20 deposits are exploited. The minerals of pyrite ores have been investigated. Results of the investigations have been presented. Symmetry constants of the minerals correspond to constants of general objects. It has been shown that the ore formation is connected with generation of magma.
dc.title	MASSIVE SULFIDE ORES OF THE URALS: A NEW GENERAL MINERALOGICAL OBJECT
dc.type	Статья

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