Earth mineralogical model: Gibbs free energy minimization computation in the system MgOFeOSiO2

Author:

Saxena S.K.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference125 articles.

1. Pyroxene-garnet solid solution equilibria in the system Mg4Si4O12Mg3Al2Si3O12 and Fe4Si4O12 at high pressures and temperatures;Akaogi;Phys. Earth Planet. Int.,1977

2. Refinement of enthalpy measurement of MgSiO3 perovskite and negative pressure-temperature slopes for perovskite-forming reactions;Akaogi;Geophys. Res. Lett.,1993

3. The Mg2SiO4 polymorphs (olivine, modified spinel and spinel)-thermodynamic properties from oxide-melt solution calorimetry, phase relations, and model of lattice vibrations;Akaogi;Amer. Mineral.,1984

4. Pyroxene-garnet transition: thermochemistry and elasticity of garnet solid solutions, and application to a pyrolite mantle;Akaogi,1987

5. Olivine modified spinel-spinel transitions in the system Mg2SiO4Fe2SiO4: Calorimetric measurements, thermochemical calculation, and geophysical application;Akaogi;J. Geophys. Res.,1989

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