Briartite
Metallic sulfide mineral From Wikipedia, the free encyclopedia
Metallic sulfide mineral From Wikipedia, the free encyclopedia
Briartite is an opaque iron-grey metallic sulfide mineral, Cu2(Zn,Fe)GeS4 with traces of Ga and Sn, found as inclusions in other germanium-gallium-bearing sulfides.[2]
Briartite | |
---|---|
General | |
Category | Mineral |
Formula (repeating unit) | Cu2(Fe,Zn)GeS4 |
IMA symbol | Btt[1] |
Strunz classification | 02.KA.10(02) |
Dana classification | 2.9.2.3.(02) |
Crystal system | Tetragonal |
Space group | 07;10 |
Unit cell | 297.46 ų |
Identification | |
Colour | Gray to gray blue; Iron-grey |
Twinning | Polysynthetic |
Mohs scale hardness | 3.5–4.5 |
Luster | Metallic; Unpolished |
Diaphaneity | Opaque |
Specific gravity | 4.337 (Calculated) |
Density | 4.337 g/cm3 (Calculated) |
Common impurities | Ga, Sn |
It was discovered at the Prince Léopold Mine, Kipushi, Shaba, Congo (Léopoldville) in 1965 by Francotte and others, and named for Gaston Briart who had studied formations at Kipushi.[3]
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