NEW DATA ON GOLD MINERALIZATION IN THE KOLYMA SECTOR OF THE PERIVOLCANIC ZONE OF THE OKHOTSK-CHUKOT VOLCANOGENIC BELT

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dc.contributor.author Sidorov V.A.
dc.contributor.author Al'shevskii A.V.
dc.contributor.author Volkov A.V.
dc.contributor.author Sidorov A.A.
dc.date.accessioned 2022-08-03T05:20:59Z
dc.date.available 2022-08-03T05:20:59Z
dc.date.issued 2004
dc.identifier https://www.elibrary.ru/item.asp?id=13465212
dc.identifier.citation Doklady Earth Sciences, 2004, 399, 9, 1212-1217
dc.identifier.issn 1028-334X
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/38457
dc.description.abstract In the Kolyma sector of the perivolcanic zone of the Okhotsk-Chukot Volcanogenic Belt (OCVB), we have discovered manifestations of an unusual complex (gold-silver-sulfide-rare metal) mineralization that can be economically feasible in the immediate future. A rather similar mineralization was recently discovered at the Arkachan deposit in the western Verkhoyansk region and near the Carlin-type deposits in northwestern Nevada (United States). Recently, new data on this type of mineralization have been reported from the Teutedzhak ore field located in the Kolyma sector of the OCVB perivolcanic zone. According to the perivolcanic zone located along the outer boundary of the OCVB is a tectonomagmatic region of the activity of Mesozoic structures in the OCVB. The Kolyma sector is confined to two regional structures (the Ayan-Yuryakh anticlinal uplift of Mesozoic structures and the overlying OCVB). Coyright
dc.title NEW DATA ON GOLD MINERALIZATION IN THE KOLYMA SECTOR OF THE PERIVOLCANIC ZONE OF THE OKHOTSK-CHUKOT VOLCANOGENIC BELT
dc.type Статья


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