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Gas-mineral equilibria and a possible geochemical model of the earth's interior
Authors:LL Perchuk
Institution:Institute of Experimental Mineralogy, U.S.S.R. Academy of Sciences, 142432 Chernogolovka (Moscow district)U.S.S.R.
Abstract:The study of the thermodynamic regime of metamorphism and magmatism has been based on mineralogical thermometry and barometry and calculations of the oxidation-reduction, hydration-dehydration and carbonatization-decarbonatization reactions. The origin of the fluids is considered in connection with the hydride-carbide-oxide structure of the earth's interior.
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