SOURCES OF ORE-FORMING FLUID IN FUMAROLES OF KUDRYAVYI VOLCANO, KURIL ISLANDS: PB ISOTOPIC COMPOSITION OF GAS CONDENSATES AND SUBLIMATE MINERALS

dc.contributor.author	Chugaev A.V.
dc.contributor.author	Yudovskaya M.A.
dc.contributor.author	Distler V.V.
dc.contributor.author	Chaplygin I.V.
dc.contributor.author	Eremina A.V.
dc.date.accessioned	2026-05-03T08:16:53Z
dc.date.issued	2007
dc.description.abstract	Kudryavyi Volcano is an example of the modern ore-forming system related to island-arc andesite volcanism. A direct study of high-temperature gas–hydrothermal process in the volcanic edifice is of fundamental significance for understanding the formation conditions of ore deposits in the modern recycling zones of the oceanic crust. This research was aimed at determining the sources of ore matter during formation of polymetal mineralization on the fumarole fields of Kudryavyi Volcano.
dc.identifier	https://elibrary.ru/item.asp?id=15292553
dc.identifier.citation	Doklady Earth Sciences, 2007, 413, 1, 216-219
dc.identifier.doi	10.1134/S1028334X07020183
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/52855
dc.title	SOURCES OF ORE-FORMING FLUID IN FUMAROLES OF KUDRYAVYI VOLCANO, KURIL ISLANDS: PB ISOTOPIC COMPOSITION OF GAS CONDENSATES AND SUBLIMATE MINERALS
dc.type	Статья

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