A thermodynamic study on the pyrite-pyrrhotite-magnetite-water system at 300–500°C with relevance to the fugacity/concentration quotient of aqueous H2S-Reference-Cited by-同舟云学术

A thermodynamic study on the pyrite-pyrrhotite-magnetite-water system at 300–500°C with relevance to the fugacity/concentration quotient of aqueous H2S

Published:1989-09 Issue:9 Volume:53 Page:2143-2155
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Klshima Noriaki

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference88 articles.

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2. Equilibrium relations between pyrrhotite and pyrite from 325° to 743°C;Arnold;Econ. Geol.,1962

3. Gas pressures in goethermal systems;Arnórsson;Chem. Geol.,1985

4. Solubility of pyrrhotite in chloride solutions at elevated temper- atures and pressures;Arutyunyan;Geochem. Intl.,1984

5. Thermodynamical Properties of Inorganic Substances;Barin,1973

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