Olivine-modified spinel-spinel transitions in the system Mg2SiO4-Fe2SiO4: Calorimetric measurements, thermochemical calculation, and geophysical application

Author:

Akaogi Masaki,Ito Eiji,Navrotsky Alexandra

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference60 articles.

1. High pressure phase equilibria in a garnet lherzolite, with special reference to Mg2+ - Fe2+ partitioning among constituent minerals;Akaogi;Phys. Earth Planet. Inter.,1979

2. The Mg2SiO4 polymorphs (olivine, modified spinel, and spinel) - Thermodynamic properties from oxide melt solution calorimetry, phase relations, and models of lattice vibrations;Akaogi;Am. Mineral.,1984

3. Geophys. Monogr. Ser.;Akimoto,1987

4. Olivine-spinel solid solution equilibria in the system Mg2SiO4- Fe2SiO4;Akimoto;J. Geophys. Res.,1968

5. The olivine-spinel transition in Fe2SiO4 and Ni2SiO4;Akimoto;J. Geophys. Res.,1965

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