The Gibbs method and Duhem's theorem: The quantitative relationships among P, T, chemical potential, phase composition and reaction progress in igneous and metamorphic systems
- 1 June 1988
- journal article
- Published by Springer Nature in Contributions to Mineralogy and Petrology
- Vol. 99 (2) , 249-256
- https://doi.org/10.1007/bf00371465
Abstract
No abstract availableKeywords
This publication has 8 references indexed in Scilit:
- Derivation of Internally-Consistent Thermodynamic Data by the Technique of Mathematical Programming: a Review with Application the System MgO-SiO2-H2OJournal of Petrology, 1986
- High temperature alteration of Abyssal ultramafics from the Islas Orcadas Fracture Zone, South AtlanticContributions to Mineralogy and Petrology, 1985
- Chemical mass transfer in magmatic processesContributions to Mineralogy and Petrology, 1985
- Quantitative P-T paths from zoned minerals: Theory and tectonic applicationsContributions to Mineralogy and Petrology, 1983
- Chapter 7. BUFFERING, INFILTRATION, and the CONTROL of INTENSIVE VARIABLES during METAMORPHISMPublished by Walter de Gruyter GmbH ,1982
- Chapter 4. ANALYTICAL FORMULATION of PHASE EQUILIBRIA: The GIBBS' METHODPublished by Walter de Gruyter GmbH ,1982
- Reactions in Amphibolite, Greenschist and BlueschistJournal of Petrology, 1982
- Theoretical prediction of equilibrium phase assemblages in multicomponent systemsAmerican Journal of Science, 1974