Thermodynamics of Minerals and Melts
Author:
Affiliation:
1. Department of Geological Sciences, AJ-20, University of Washington, Seattle, WA 98195.
Funder
National Sleep Foundation
Publisher
Wiley
Subject
Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1002/rog.1991.29.s2.446
Reference623 articles.
1. The relationship between the adiabatic bulk modulus and enthalpy for mantle-related minerals
2. Formulation of the thermodynamic functions for mantle minerals: MgO as an example
3. Internally-consistent thermodynamic data for minerals in the system Na2O-K2O-CaO-MgO-FeO-Fe2O3-Al2O3-SiO2-TiO2-H2O-CO2;Berman R. G.;J. Penal.,1988
4. Derivation of Internally-Consistent Thermodynamic Data by the Technique of Mathematical Programming: a Review with Application the System MgO-SiO2-H2O
5. Estimating the thermodynamic properties (GD f and ∆HD f) of silicate minerals at 298 K from she sum of polyhedral contributions;Chermak J. A.;Amer. Mineral.,1989
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1. Harzburgite melting with and without H2O: Experimental data and predictive modeling;Journal of Geophysical Research: Solid Earth;2004-02
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