PORPHYRY COPPER DEPOSITS OF THE CIS AND THE MODELS OF THEIR FORMATION

dc.contributor.author	Zvezdov V.S.
dc.contributor.author	Migachev I.F.
dc.contributor.author	Girfanov M.M.
dc.date.accessioned	2020-11-10T07:19:28Z
dc.date.available	2020-11-10T07:19:28Z
dc.date.issued	1993
dc.identifier	https://elibrary.ru/item.asp?id=31145454
dc.identifier.citation	Ore Geology Reviews, 1993, , 6, 511-549
dc.identifier.issn	0169-1368
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/18901
dc.description.abstract	Deposits of the “porphyry” family (essentially porphyry copper and gold-porphyry copper, gold-bearing porphyry molybdenum-copper, gold-containing porphyry copper-molybdenum and porphyry molybdenum deposits) are associated in time and space with granitoid magmatism mainly in Phaerozoic volcano-plutonic belts. Whatever their age, the deposits belong to two types of belts: basaltic belts, representing axial zones of island arcs, or andesitic belts formed within active continental (Andean-type) margins.
dc.title	PORPHYRY COPPER DEPOSITS OF THE CIS AND THE MODELS OF THEIR FORMATION
dc.type	Статья

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