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

Volkov A.V.; Prokof'ev V.Y.; Sidorov A.A.

dc.contributor.author	Volkov A.V.
dc.contributor.author	Prokof'ev V.Y.
dc.contributor.author	Sidorov A.A.
dc.date.accessioned	2024-11-02T11:07:55Z
dc.date.available	2024-11-02T11:07:55Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13524293
dc.identifier.citation	Doklady Earth Sciences, 2006, 408, 4, 513-517
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46372
dc.description.abstract	According 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.subject	Promezhutochnoe deposit
dc.subject	Chukotka
dc.title	NEW DATA ON FORMATION CONDITIONS AND COMPOSITION OF ORE-FORMING FLUIDS IN THE PROMEZHUTOCHNOE GOLD-SILVER DEPOSIT (CENTRAL CHUKOTKA, RUSSIA)
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06040015