The effect of Al 2 O 3 on Fe-Mg partitioning between magnesiowüstite and magnesium silicate perovskite

By D. Frost, F. Langenhorst. 2002

193 citations recorded by the source corpus.

Subfields: Geophysics, Materials Chemistry

View Paper: https://www.semanticscholar.org/paper/4a979d8c244e458c073c39f4133d087b0ee64a60

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In Geophysics

1. Y. Ricard
2. J. Matas
3. E. Mattern
4. Feiwu Zhang
5. Artem R. Oganov
6. J. Bass
7. K. Hirose
8. D. Bercovici

In Materials Chemistry

1. Artem R. Oganov
2. Feiwu Zhang
3. J. Bass

Citations in the corpus

• Lower mantle composition and temperature from mineral physics and thermodynamic modelling (2005, background): “(5) It has been reported that in Al2O3 -free systems, Fe preferentially partitions into magnesiowustite rather than into perovskite giving values of KD around 0.25 (Katsura & Ito 1996; Mao et al. 1997; Martinez et al. 1997; Frost & Langenhorst 2002).”
• Valence state and spin transitions of iron in Earth's mantle silicates (2006, background): “For Pv we find that [Fe–Al] coupled substitutions are favourable, in agreement with previous studies [2,3,8].”