Oxygen regime of granulite metamorphism: Modeling by the method of Gibbs free energy minimization

Data on the component composition and acid-base properties of cooling fluid in the systems H 2 O-CO 2 , H 2 O-NaCl, and H 2 O-rock forming minerals, which were derived by minimizing the Gibbs free energy, and the evaluated contributions of major fluid components to its acid-base properties suggest that the main reason for the inversion of acid-base properties of magmatic fluids in the fluid-granite system is the opposite tendencies in the changes of the dissociation constants of acidic and basic fluid components in the course of fluid cooling.

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Oxygen regime of granulite metamorphism: Modeling by the method of Gibbs free energy minimization

Cited by 2 publications

References 4 publications

Possibility of estimating acid-base properties of minerals and rocks by means of physicochemical simulations (with the Selector-C program package)

Possibility of estimating acid-base properties of minerals and rocks by means of physicochemical simulations (with the Selector-C program package)

Acid-base properties of cooling magmatic fluid and D.S. Korzhinskii’s “acidic wave” mechanism: Physicochemical simulation results

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