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1971•International Geology ReviewRequires access

Theory of metasomatic zonation with parallel reactions

В. С. Голубев

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Abstract

A mathematical model of infiltrational and diffusional metasomatism, based on equations of the balance of substance and kinetics of the accompanying reactions between the solutes and the rocks, shows that a system of mineralogically different metasomatic zones develops during filtration and diffusion of hydrothermal solutions; in the infiltrational metasomatism, if the reactions are rapid, the interzonal boundaries are strikingly definite, but no such definite boundaries can be developed in the diffusional metasomatism. V.P. Sokoloff.

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A mathematical model of infiltrational and diffusional metasomatism, based on equations of the balance of substance and kinetics of the accompanying reactions between the solutes and the rocks, shows that a system of mineralogically different metasomatic zones develops during filtration and diffusion of hydrothermal solutions; in the infiltrational metasomatism, if the reactions are rapid, the interzonal boundaries are strikingly definite, but no such definite boundaries can be developed in the diffusional metasomatism. V.P. Sokoloff.

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Available abstract

A mathematical model of infiltrational and diffusional metasomatism, based on equations of the balance of substance and kinetics of the accompanying reactions between the solutes and the rocks, shows that a system of mineralogically different metasomatic zones develops during filtration and diffusion of hydrothermal solutions; in the infiltrational metasomatism, if the reactions are rapid, the interzonal boundaries are strikingly definite, but no such definite boundaries can be developed in the diffusional metasomatism. V.P. Sokoloff.

Key concepts: Metasomatism, Hydrothermal circulation, Geology, Diffusion, Geochemistry, Kinetics, Thermodynamics, Physics

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