Nichromite
Nichromite (Ni,Co,Fe)(Cr,Fe,Al)2O4[1] is a black cubic metallic mineral and member of the spinel group.[5] Nichromite was originally reported from the Bon Accord nickel deposit in Barberton District, South Africa.[1] Occurring naturally in a nickel deposit, nichromite is named for chromite with dominant nickel.[2]
Nichromite | |
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General | |
Category | Spinel group |
Formula (repeating unit) | (Ni,Co,Fe)(Cr,Fe,Al)2O4 |
Strunz classification | 4.BB.05 |
Crystal system | Isometric |
Crystal class | Hexoctahedral (m3m) H-M symbol: (4/m 3 2/m) |
Space group | Fd3m |
Unit cell | a = 8.32 Å; V = 573.86 Å3; Z = 8 |
Identification | |
Color | Dark green, black |
Crystal habit | Granular, anhedral to subhedral |
Fracture | Conchoidal |
Mohs scale hardness | 6-6 1⁄2 |
Luster | Metallic |
Streak | Greyish green |
Diaphaneity | Opaque |
Specific gravity | 5.10 |
Optical properties | Isotropic |
References | [1][2][3][4] |
The atomic arrangement of the spinel group is a commonly studied structure and characteristically has four closely packed oxygen atoms. The nickel atoms are organized corresponding to a "normal" spinel arrangement.[6]
The mineral has only been found in the Bon Accord Nickel Deposit in South Africa where it is formed by replacing chromite and rimmed by trevorite.[4]
References
- Nichromite on Mindat.org
- Nichromite on Webmineral
- Sawaokaa,A.,Saitoa,S.,Inoueb,K. and Asadab,T. (1971)Effect of high pressure on the lattice constants of chromites having the spinel structure. Materials Research Bulletin, 6, 97-101.
- Cabri, L. J., Chao G.Y., Pabst, Adolf, Fleischer, Michael. (1980) New Mineral Names. American Mineralogist, 65, 811.
- Glossary of Geology
- Wyckoff, R.W.G. (1965) Crystal Structures (Second Edition). 75-86 p. University of Arizona, Tucson, Arizona.
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