NEW DATA ON FORMATION CONDITIONS AND COMPOSITION OF ORE-FORMING FLUIDS IN THE PROMEZHUTOCHNOE GOLD-SILVER DEPOSIT (CENTRAL CHUKOTKA, RUSSIA)

dc.contributor.authorVolkov A.V.
dc.contributor.authorProkof'ev V.Y.
dc.contributor.authorSidorov A.A.
dc.date.accessioned2024-11-02T11:07:55Z
dc.date.available2024-11-02T11:07:55Z
dc.date.issued2006
dc.description.abstractAccording to the conventional concept based on a great body of empirical data, volcanogenic or epithermal deposits do not grade into mesothermal or plutonogenic ones with depth. However, in the Maisk ore group of central Chukotka, epithermal Promezhutochnoe (Northeast), Sil’noe, and Sopka Rudnaya gold–silver deposits have been discovered in terrigenous flysch sequences at the basement of the Okhotsk–Chukot volcanogenic belt (OCVB).
dc.identifierhttps://www.elibrary.ru/item.asp?id=13524293
dc.identifier.citationDoklady Earth Sciences, 2006, 408, 4, 513-517
dc.identifier.doi10.1134/S1028334X06040015
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/46372
dc.subjectPromezhutochnoe deposit
dc.subjectChukotka
dc.titleNEW DATA ON FORMATION CONDITIONS AND COMPOSITION OF ORE-FORMING FLUIDS IN THE PROMEZHUTOCHNOE GOLD-SILVER DEPOSIT (CENTRAL CHUKOTKA, RUSSIA)
dc.typeСтатья

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