Evaluation of (Mg,Fe) partitioning between silicate perovskite and magnesiowustite up to 120 GPa and 2300 K

Author:

Andrault Denis

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

Reference36 articles.

1. Anharmonicity and the equation of state for gold;Anderson;J. Appl. Phys.,1989

2. High pressure phase transformations in the MgFe2O4 and Fe2O3-MgSiO3 systems;Andrault;Phys. Chem. Miner.,2000

3. Pressure-induced landau-type transition in stishovite;Andrault;Science,1998

4. A versatile diamond anvil cell for IR spectroscopy and X-ray diffraction analysis;Chervin;Rev. Sci. Instrum.,1995

5. P-V-T equation of state if magnesiowustite (Mg0.6,Fe0.4)O;Fei;Phys. Chem. Miner.,1992

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