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dolomite |
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dolomite [ˈdɒləˌmaɪt] n 1. (Earth Sciences / Minerals) a white mineral often tinted by impurities, found in sedimentary rocks and veins. It is used in the manufacture of cement and as a building stone (marble). Composition: calcium magnesium carbonate. Formula: CaMg(CO3)2. Crystal structure: hexagonal (rhombohedral) 2. (Earth Sciences / Geological Science) a sedimentary rock resembling limestone but consisting principally of the mineral dolomite. It is an important source of magnesium and its compounds, and is used as a building material and refractory [named after Déodat de Dolomieu (1750-1801), French mineralogist] dolomitic [ˌdɒləˈmɪtɪk] adj
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3] of brackish to fresh groundwaters (the former containing about 10% seawater) would be required to dolomitize one cubic metre of limestone with an initial porosity of 40%, or 650 [m. |
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