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]...
Main Authors: | , , , , , , , |
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Other Authors: | |
Format: | Article |
Language: | English |
Published: |
National Academy of Sciences,
2009-12-28T14:55:27Z.
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Subjects: | |
Online Access: | Get fulltext |