Calcite-dolomite-magnesite stability relations in solutions: the effect of ionic strength

Physics

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Scientific paper

The effect of total solution concentration on the Ca: Mg ratio at the magnesitedolomite and the dolomite-calcite boundaries in CaCl 2 ---MgCl 2 ---CO 2 solutions has been determined between 280 and 420°C. Below about 410° a decrease in the total concentration of the solutions produces a displacement of both boundaries toward lower values of the Ca:Mg ratio. Observed displacements are small but increase with decreasing temperature.

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