PHANEROZOIC COPPER AND PRECIOUS METAL ORE FORMATIONS OF THE EAST EUROPEAN PLATFORM

dc.contributor.author	Chaikin V.G.
dc.contributor.author	Glebashev S.G.
dc.contributor.author	Meskhi A.M.
dc.contributor.author	Zakirova F.A.
dc.date.accessioned	2022-10-01T05:54:58Z
dc.date.available	2022-10-01T05:54:58Z
dc.date.issued	2004
dc.identifier	https://elibrary.ru/item.asp?id=13472270
dc.identifier.citation	Geology of Ore Deposits, 2004, 46, 6, 479-487
dc.identifier.issn	1075-7015
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38860
dc.description.abstract	Based on ore-formation analysis, the distribution and deposition conditions of exogenic copper and precious metal (Ag, Pt, Pd, Au) ores within the sedimentary cover of the East European Platform are examined. Three main ore formations are defined: copper, precious metal-copper, and precious metal. Their deposition in metallogenic zones with different mineralization was determined by tectonomagmatic activation during the Caledonian, Hercynian, and Alpine stages of the platform development. The Hercynian stage was characterized by the minimal scale of stratiform mineralization and the widest metallogenic profile of copper and precious metals. Of the main geodynamic settings, represented by continental rifts, interrift blocks, and superimposed marginal troughs, interrift blocks were most favorable for the formation of commercial hydrogene mineralization.
dc.title	PHANEROZOIC COPPER AND PRECIOUS METAL ORE FORMATIONS OF THE EAST EUROPEAN PLATFORM
dc.type	Статья

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