Bornite | |
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General | |
Category | Sulfide mineral |
Formula (repeating unit) | Cu5FeS4 |
IMA symbol | Bn[1] |
Strunz classification | 2.BA.10 |
Crystal system | Orthorhombic |
Crystal class | Dipyramidal (mmm) H-M symbol: (2/m 2/m 2/m) |
Space group | Pbca |
Unit cell | a = 10.95 Å, b = 21.862 Å, c = 10.95 Å; Z = 16 |
Identification | |
Formula mass | 501.88 g/mol |
Color | Copper red, bronze brown, purple |
Crystal habit | Granular, massive, disseminated – Crystals pseudocubic, dodecahedral, octahedral |
Twinning | Penetration twins on [111] |
Cleavage | Poor on [111] |
Fracture | Uneven to subconchoidal |
Tenacity | Brittle |
Mohs scale hardness | 3–3.25 |
Luster | Metallic if fresh, iridescent tarnish |
Streak | Grayish black |
Specific gravity | 5.06–5.08 |
Refractive index | Opaque |
Pleochroism | Weak but noticeable |
Other characteristics | Magnetic after heating, iridescent |
References | [2][3][4] |
Bornite, also known as peacock ore, is a sulfide mineral with chemical composition Cu5FeS4 that crystallizes in the orthorhombic system (pseudo-cubic).