Partitioning of iron between magnesian silicate perovskite and magnesiowüstite at about 1 Mbar-Reference-Cited by-同舟云学术

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Partitioning of iron between magnesian silicate perovskite and magnesiowüstite at about 1 Mbar

Published:2002-08 Issue:3-4 Volume:131 Page:295-310
ISSN:0031-9201
Container-title:Physics of the Earth and Planetary Interiors
language:en
Short-container-title:Physics of the Earth and Planetary Interiors

Author:

Kesson S.E,Fitz Gerald J.D,O’Neill H.St.C,Shelley J.M.G

Publisher

Elsevier BV

Subject

Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics

Reference51 articles.

1. Evaluation of (Mg, Fe) partitioning between silicate perovskite and magnesiowüstite up to 120 GPa and 2300 K;Andrault;J. Geophys. Res.,2001

2. Internally consistent thermodynamic data and equilibrium phase relations for compounds in the system MgO–SiO2 at high pressure;Fei;J. Geophys. Res.,1990

3. Experimental determination of element partitioning and calculation of phase relations in the MgO–FeO–SiO2 system at high pressure and high temperature;Fei;J. Geophys. Res.,1991

4. Temperature-dependent electron delocalization in (Mg, Fe)SiO3 perovskite;Fei;Am. Miner.,1994

5. Maximum solubility of FeO in (Mg, Fe)SiO3-perovskite as a function of temperature at 26 GPa: implication for FeO content in the lower mantle;Fei;J. Geophys. Res.,1996

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