RELATION BETWEEN PORPHYRY DEPOSITS AND THEIR VEIN SATELLITES

dc.contributor.author	Sidorov A.A.
dc.contributor.author	Tomson I.N.
dc.contributor.author	Savva N.E.
dc.contributor.author	Volkov A.V.
dc.contributor.author	Prokof'ev V.Yu.
dc.contributor.author	Kolova E.E.
dc.date.accessioned	2024-10-19T07:54:47Z
dc.date.available	2024-10-19T07:54:47Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13505429
dc.identifier.citation	Doklady Earth Sciences, 2006, 409, 6, 859-863
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46063
dc.description.abstract	Porphyry copper, molybdenum, tin, tin–silver, gold–rare metal and other deposits are commonly accompanied by nonporphyry ore formations that are frequently similar to the entire porphyry group. They are represented by sulfide–quartz (base metal), gold–sulfide–quartz, epithermal gold–silver, antimony, and mercury deposits of vein and stringer–disseminated ores. The detailed study of such satellite deposits revealed that they have mineralogical–geochemical links with the basic porphyry ores. However, the porphyry and nonporphyry deposits seem to be of the same type in some places because of similar physicochemical constraints of vein formation.
dc.subject	porphyry deposits
dc.title	RELATION BETWEEN PORPHYRY DEPOSITS AND THEIR VEIN SATELLITES
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06060043

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