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, Bengtson, Amelia, Morgan, Dane, Sturhahn, Wolfgang, Catalli, Krystle C., Zhao, Jiyong, Lerche, Michael, Prakapenka, Vitali
Other Authors: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Format: Article
Language:en_US
Published: National Academy of Sciences 2009
Online Access:http://hdl.handle.net/1721.1/50247

Internet

http://hdl.handle.net/1721.1/50247

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