Fig. 5: Saturation indices of major carbon-bearing minerals. | Communications Earth & Environment

Fig. 5: Saturation indices of major carbon-bearing minerals.

From: Rapid mineralisation of carbon dioxide in peridotites

Fig. 5

Calculated saturation indices (SI) of the collected fluid samples with respect to calcite, hydromagnesite, dolomite and magnesite. Positive, negative and zero SI values correspond to the fluids being supersaturated, undersaturated and at equilibrium with the specific mineral.

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