
AbstractA short review on the chemical composition of underground brines is presented. Diagrams of brine saturation of upper-saline, saline, and under-saline formations have been determined with respect to common minerals of the water-bearing rock. It is shown that even brines of 300-500 g/dm3 are not equilibrated with primary (endogenic) minerals, as they all continue to react.
Underground brines, Geochemistry, Chemical interaction, Equilibrium, Rock, Earth and Planetary Sciences(all)
Underground brines, Geochemistry, Chemical interaction, Equilibrium, Rock, Earth and Planetary Sciences(all)
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