Dolomite | |
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General | |
Category | Carbonate minerals |
Formula (repeating unit) | CaMg(CO3)2 |
IMA symbol | Dol[1] |
Strunz classification | 5.AB.10 |
Crystal system | Trigonal |
Crystal class | Rhombohedral (3) H–M symbol: (3) |
Space group | R3 |
Unit cell | a = 4.8012(1), c = 16.002 [Å]; Z = 3 |
Identification | |
Color | White, grey to pink, reddish-white, brownish-white; colourless in transmitted light |
Crystal habit | Tabular crystals, often with curved faces, also columnar, stalactitic, granular, massive. |
Twinning | Common as simple contact twins |
Cleavage | 3 directions of cleavage not at right angles |
Fracture | Conchoidal |
Tenacity | Brittle |
Mohs scale hardness | 3.5–4.0 |
Luster | Vitreous to pearly |
Streak | White |
Specific gravity | 2.84–2.86 |
Optical properties | Uniaxial (−) |
Refractive index | nω = 1.679–1.681 nε = 1.500 |
Birefringence | δ = 0.179–0.181 |
Solubility | Poorly soluble in dilute HCl |
Other characteristics | May fluoresce white to pink under UV; triboluminescent. Ksp values vary between 10−19 and 10−17 |
References | [2][3][4][5][6] |
Dolomite (/ˈdɒl.əˌmaɪt, ˈdoʊ.lə-/) is an anhydrous carbonate mineral composed of calcium magnesium carbonate, ideally CaMg(CO3)2. The term is also used for a sedimentary carbonate rock composed mostly of the mineral dolomite (see Dolomite (rock)). An alternative name sometimes used for the dolomitic rock type is dolostone.