Tetrahedrite | |
---|---|
General | |
Category | Sulfosalt mineral |
Formula (repeating unit) | (Cu,Fe) 12Sb 4S 13 |
Strunz classification | 2.GB.05 |
Crystal system | Cubic |
Crystal class | Hextetrahedral (43m) H-M symbol: (4 3m) |
Space group | I43m |
Unit cell | a = 10.39(16) Å; Z = 2 |
Identification | |
Color | Steel gray to iron-gray |
Crystal habit | Groups of tetrahedral crystals; massive, coarse to fine compact granular |
Twinning | Contact and penetration twins on {111} |
Cleavage | None |
Fracture | Uneven to subconchoidal |
Tenacity | Somewhat brittle |
Mohs scale hardness | 3+1⁄2 – 4 |
Luster | Metallic, commonly splendent |
Streak | Black, brown to dark red |
Diaphaneity | Opaque, except in very thin fragments |
Specific gravity | 4.97 |
Optical properties | Isotropic |
Refractive index | n greater than 2.72 |
References | [1][2] |
Tetrahedrite is a copper antimony sulfosalt mineral with formula: (Cu,Fe)
12Sb
4S
13. It is the antimony endmember of the continuous solid solution series with arsenic-bearing tennantite. Pure endmembers of the series are seldom if ever seen in nature. Of the two, the antimony rich phase is more common. Other elements also substitute in the structure, most notably iron and zinc, along with less common silver, mercury and lead. Bismuth also substitutes for the antimony site and bismuthian tetrahedrite or annivite is a recognized variety. The related, silver dominant, mineral species freibergite, although rare, is notable in that it can contain up to 18% silver.