VELIKITE, CU2HGSNS4, THE MERCURY MEMBER OF THE STANNITE GROUP

Show simple item record

dc.contributor.author Spiridonov E.M.
dc.contributor.author Gruzdev V.S.
dc.contributor.author Volgin V.Y.
dc.contributor.author Kaplunnik L.N.
dc.contributor.author Pobedimskaya Y.A.
dc.contributor.author Chvileva T.N.
dc.contributor.author Chernitsova N.M.
dc.date.accessioned 2020-04-10T02:20:29Z
dc.date.available 2020-04-10T02:20:29Z
dc.date.issued 1988
dc.identifier https://elibrary.ru/item.asp?id=30956114
dc.identifier.citation TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1988, 300, 3, 116-119
dc.identifier.issn 0891-5571
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/16531
dc.description.abstract In the middle of the 1970's in the Khaydarkan antimony-mercury deposit, Kirgizia, one of the present writers (Volgin) found a new copper-mercury-tin sulfide. It was called velikite after A.S. Velikiy. The composition of the velikite specimen whose structure had been established was later determined more accurately by microprobe analysis. Velikite in the Khaydarkan deposit forms small grains and crystals of tetragonal-scalenohedral habit, no larger than 1 mm. It is associated with stibnite, metacinnabarite, aktashite, livingstonite, quartz and fluorite. The mineral has a dark-gray color; the luster is metallic, and the streak gray. These and other properties of the mineral, including chemical composition, are discussed and lead to the conclusion that velikite is the mercury member of the stannite group.
dc.title VELIKITE, CU2HGSNS4, THE MERCURY MEMBER OF THE STANNITE GROUP
dc.type Статья


Files in this item

Files Size Format View

There are no files associated with this item.

This item appears in the following Collection(s)

  • ELibrary
    Метаданные публикаций с сайта https://www.elibrary.ru

Show simple item record