Barbertonite | |
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General | |
Category | Carbonate mineral |
Formula (repeating unit) | Mg6(Cr,Al)2(OH)16CO3·4H2O |
Strunz classification | 5.DA.45 |
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 = 6.17 Å, c = 15.52 Å; Z = 1 |
Identification | |
Color | Intense violet to rose-pink |
Crystal habit | flattened plates, in fibrous matted masses, and as cross-fiber veinlets |
Cleavage | Perfect on {0001} |
Tenacity | Flexible but not elastic |
Mohs scale hardness | 1+1⁄2–2 |
Luster | Waxy, pearly |
Streak | Very pale violet to white |
Diaphaneity | Transparent |
Specific gravity | 2.05–2.15 |
Optical properties | Uniaxial (−) may appear biaxial due to strain |
Refractive index | nω = 1.557 nε = 1.529 |
Birefringence | δ = 0.028 |
Pleochroism | Weak, O = dark rose-pink to violet; E = pale rose-pink to violet |
References | [1][2][3] |
Barbertonite is a magnesium chromium carbonate mineral with formula of Mg6Cr2(OH)16CO3·4H2O. It is polymorphous with the mineral stichtite and, along with stichtite, is an alteration product of chromite in serpentinite. Barbertonite has a close association with stichtite, chromite, and antigorite (Taylor, 1973).[4] Mills et al. (2011) presented evidence that barbertonite is a polytype of stichtite and should be discredited as a mineral species.[5]