MAIKAINITE CU20(FE,CU 6MO2GE6S32 AND OVAMBOITE CU20(FE,CU,ZN )6W2GE6S32: NEW MINERALS IN MASSIVE SULFIDE BASE METAL ORES
- DSpace Home
- →
- Геология России
- →
- ELibrary
- →
- View Item
JavaScript is disabled for your browser. Some features of this site may not work without it.
dc.contributor.author | Spiridonov E.M. | |
dc.date.accessioned | 2022-01-16T05:05:33Z | |
dc.date.available | 2022-01-16T05:05:33Z | |
dc.date.issued | 2003 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=13443644 | |
dc.identifier.citation | Doklady Earth Sciences, 2003, 393, 9, 1329-1332 | |
dc.identifier.issn | 1028-334X | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/34354 | |
dc.description.abstract | In addition to molybdenite, tungstenite, and iordisit, complex sulfides of Mo and W (hemusite, kiddcreekite, castanite, Mo- and W-containing colusite, Ge-colusIte, and germanite) have been detected in hydrothermal ores. The standard pink germanite contains trace~ of Mo and W, while the yellowish modification contams as much as 1-3% Wand/or Mo [2-15]. In ores from. ~assive sulfide base metal deposits (Tsumeb, Namibia; Maikain, Kazakhstan), researchers have found complex sulfides of Cu(Fe,Zn), Ge(As,Ga), and (Mo:W) [4, 12] associated with bornite, sphalerite, tennanttte, gerrnanite CU20(Cu,Fe,Zn)6Fe2(Ge,As,Ga)6Se32 [3],. C!e-colusite CU20(Cu,Fe,Zn)6V2(Ge,As)6Se32 [5], remente, Ge-mawsonite, Ge-briartite, sulvanite, and others. The Mo-dominated mineral was named maikainite ~ter the locality of its first finding, whereas the W-dommated modification was named ovamboite after the Ovamboland region hosting the Tsumeb deposit (Namibia). | |
dc.subject | Maikainite | |
dc.subject | Ovamboite | |
dc.title | MAIKAINITE CU20(FE,CU 6MO2GE6S32 AND OVAMBOITE CU20(FE,CU,ZN )6W2GE6S32: NEW MINERALS IN MASSIVE SULFIDE BASE METAL ORES | |
dc.type | Статья |
Files in this item
This item appears in the following Collection(s)
-
ELibrary
Метаданные публикаций с сайта https://www.elibrary.ru