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Magnesite (MgCO3) and dolomite (MgCa(CO3)2) are the most stable carbonate minerals under typical Earth surface conditions, with the highest resistance to leaching and weathering. Their dissolution rates are for example 100–1000 times lower than that of calcite in a wide range of conditions, from ambient temperature to 150 °C and pH from 1 to 14 (Pokrovski et al., 2009).
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