Oxide-metal equilibria to 2500°C and 25 GPa: Implications for core formation and the light component in the Earth's core

Author:

O'Neill Hugh St. C.,Canil Dante,Rubie David C.

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

Reference72 articles.

1. Constraints on core composition from shock-wave data;Ahrens;Philos Trans. R. Soc. London. Ser. A,1982

2. Activities of components in oxide solid solutionsaethe systems CoO-MgO, CoO-MnO, and CoO-'FeO' at 1200°C.;Aukrust;Trans. Metall. Soc. AIME,1963

3. Density and composition of mantle and core;Birch;J. Geophys. Res.,1964

4. Temperatures in the Earth's core from melting-point measurements of iron at high static pressures;Boehler;Nature,1993

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