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dc.contributor.author Kulikova I.M.
dc.contributor.author Vershkovskaya O.V.
dc.contributor.author Blinov V.A.
dc.contributor.author Chvileva T.N.
dc.contributor.author Gorshkov Y.N.
dc.date.accessioned 2020-04-10T02:18:09Z
dc.date.available 2020-04-10T02:18:09Z
dc.date.issued 1988
dc.identifier https://elibrary.ru/item.asp?id=30955198
dc.identifier.citation TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1988, 303, 6, 115-118
dc.identifier.issn 0891-5571
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/16496
dc.description.abstract Until now, no descriptions of duranusite in Soviet deposits have been published. We found this mineral in a mercury-antimony deposit in central Tadzhikistan, whose ores are localized in complexly-deformed clastic rocks of Middle to Late Carboniferous age, intruded by granitoid stocks and dikes. The mineralization is controlled by a large fault, along which limestones of Middle Devonian to Early Carboniferous age are thrust over the sandstone-shale sequence. The host rocks are highly silicified, dickitized, sericitized and pyritized. The mineral composition of the area of this deposit is fairly complex and includes several successively formed paragenetic mineral associations.
dc.subject Devonian en
dc.subject Carboniferous en
dc.title DURANUSITE FROM A MERCURY-ANTIMONY DEPOSIT OF CENTRAL TADZHIKISTAN
dc.type Статья
dc.subject.age Paleozoic::Devonian en
dc.subject.age Paleozoic::Carboniferous en
dc.subject.age Палеозой::Девонская ru
dc.subject.age Палеозой::Каменноугольная ru


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