Electronic and magnetic structures of the postperovskite-type Fe[subscript 2]O[subscript 3] and implications for planetary magnetic records and deep interiors

Electronic and magnetic structures of the postperovskite-type Fe[subscript 2]O[subscript 3] and implications for planetary magnetic records and deep interiors

Recent studies have shown that high pressure (P) induces the metallization of the Fe[superscript 2+]-O bonding, the destruction of magnetic ordering in Fe, and the high-spin (HS) to low-spin (LS) transition of Fe in silicate and oxide phases at the deep planetary interiors. Hematite (Fe[subscript 2]...

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Bibliographic Details
Main Authors: Shim, Sang-Heon Dan (Contributor), Bengtson, Amelia (Author), Morgan, Dane (Author), Sturhahn, Wolfgang (Author), Catalli, Krystle C. (Contributor), Zhao, Jiyong (Author), Lerche, Michael (Author), Prakapenka, Vitali (Author)
Other Authors: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences (Contributor)
Format: Article
Language:English
Published: National Academy of Sciences, 2009-12-28T14:55:27Z.
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