Physics
Scientific paper
Dec 1989
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1989georl..16.1399w&link_type=abstract
Geophysical Research Letters (ISSN 0094-8276), vol. 16, Dec. 1989, p. 1399-1402.
Physics
6
Computerized Simulation, Earth Mantle, Iron, Magnesium Compounds, Perovskites, Silicates, Abundance, Metal Ions, Single Crystals
Scientific paper
Atomistic computer simulation techniques are used to study site partitioning of iron in (Mg,Fe)SiO2 perovskites. The calculations predict that the most energetically favorable reaction for iron substitution is the direct exchange of Fe(2+) for Mg(2+). It is concluded that the substitution of Fe into the octahedral site and Si into the 8-12 fold coordinated site (Jackson et al., 1987) is unlikely.
Price Geoffrey D.
Wright Kate
No associations
LandOfFree
Computer simulations of iron in magnesium silicate perovskite does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.
If you have personal experience with Computer simulations of iron in magnesium silicate perovskite, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Computer simulations of iron in magnesium silicate perovskite will most certainly appreciate the feedback.
Profile ID: LFWR-SCP-O-1570315