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Dolomite (CaCO3MgCO3) is a sedimentary rock occurs as a sedimentary deposit similar in nature to limestone. Most dolomite deposits are as a result of replacement of Mg instead of Ca during the recrystallization of limestone (Dolomitzation), while some dolomite precipitates directly from seawater. The dolomite rocks contain more than 50% of both calcite and dolomite minerals in which dolomite is more abundant than calcite.


Dolomite Report



Dolomite Brouchure