Nickeline | |
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General | |
Category | Arsenide mineral |
Formula (repeating unit) | nickel arsenide (NiAs) |
IMA symbol | Nc[1] |
Strunz classification | 2.CC.05 |
Crystal system | Hexagonal |
Crystal class | Dihexagonal dipyramidal (6/mmm) H-M symbol: (6/m 2/m 2/m) |
Space group | P63/mmc |
Unit cell | a = 3.602 Å, c = 5.009 Å; Z = 2 |
Identification | |
Color | Pale copper red with blackish tarnish. white with strong yellowish pink hue on polished section strongly anisotropic |
Crystal habit | Massive columnar to reniform, rarely as distorted, horizontally striated, {1011} terminated crystals |
Twinning | On {1011} producing fourlings |
Cleavage | {1010} Imperfect, {0001} Imperfect |
Fracture | Conchoidal |
Tenacity | Brittle |
Mohs scale hardness | 5 – 5.5 |
Luster | metallic |
Streak | brownish black |
Diaphaneity | Opaque |
Specific gravity | 7.8 |
Pleochroism | Strong (reflected light) |
Fusibility | 2 |
Other characteristics | garlic odor on heating |
References | [2][3][4] |
Nickeline or niccolite is the mineral form of nickel arsenide. The naturally-occurring mineral contains roughly 43.9% nickel and 56.1% arsenic by mass, but composition of the mineral may vary slightly.[2]
Small quantities of sulfur, iron and cobalt are usually present, and sometimes the arsenic is largely replaced by antimony. This last forms an isomorphous series with breithauptite (nickel antimonide).