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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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2004, Conceptual models for burrow-related, selective dolomitization with textural and isotopic evidence from the Tyndall Stone, Canada: Geobiology, v. Dolomitization of the Wabamun is clearly associated with faulting at Saddle Hills and it is expected the case will be the same at Woking. Cementation, dissolution, and dolomitization require significant flow of groundwater (of whatever type and/or salinity, ranging from fresh to hypersaline), driven by an externally imposed hydraulic gradient. |
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