Pentlandite | |
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General | |
Category | Sulfide mineral |
Formula (repeating unit) | iron nickel sulfide: (Fe,Ni)9S8 |
IMA symbol | Pn[1] |
Strunz classification | 2.BB.15a |
Dana classification | 2.7.1.1 |
Crystal system | Isometric |
Crystal class | Hexoctahedral (m3m) H-M symbol: (4/m 3 2/m) |
Space group | Fm3m |
Unit cell | a = 9.928 Å, Z = 4 |
Identification | |
Formula mass | 771.94 g/mol |
Color | Yellowish bronze |
Crystal habit | Hexoctahedral rare; massive to granular |
Cleavage | Absent – octahedral parting on {111} |
Fracture | Conchoidal |
Tenacity | Brittle |
Mohs scale hardness | 3.5–4 |
Luster | Metallic |
Streak | Light bronze-brown[2][3][4][5] Greenish black[6][7][8] |
Diaphaneity | Opaque |
Specific gravity | 4.6–5.0 |
Density | 4.6–5 g/cm3 |
Fusibility | 1.5–2 |
Other characteristics | Becomes magnetic upon heating |
References | [9][2][3][4][5][6][7][8] |
Pentlandite is an iron–nickel sulfide with the chemical formula (Fe,Ni)9S8. Pentlandite has a narrow variation range in nickel to iron ratios (Ni:Fe), but it is usually described as 1:1. In some cases, this ratio is skewed by the presence of pyrrhotite inclusions. It also contains minor cobalt, usually at low levels as a fraction of weight.
Pentlandite forms isometric crystals, but it is normally found in massive granular aggregates. It is brittle with a hardness of 3.5–4 and specific gravity of 4.6–5.0 and is non-magnetic. It has a yellowish bronze color and a metallic luster.[10]
Pentlandite is found in abundance within ultramafic rocks, making it one of the most important sources of mined nickel.[11] It also occasionally occurs within mantle xenoliths and "black smoker" hydrothermal vents.[12]