Abstract
We use atomistic computer simulation techniques to investigate the site partitioning of iron in (Mg,Fe)SiO3 perovskites. Our calculations predict that the most energetically favourable reaction for iron substitution will be a direct exchange of Fe2+ for Mg2+. Substitution of Fe into the octahedral site and Si into the 8–12 fold coordinated site, as proposed by Jackson et al. [1987], is predicted to be extremely unlikely. Copyright 1989 by the American Geophysical Union.
Original language | English |
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Pages (from-to) | 1399-1402 |
Journal | Geophysical Research Letters |
Volume | 16 |
Issue number | 12 |
DOIs | |
Publication status | Published - Dec 1989 |
Externally published | Yes |