Electronic and magnetic structures of the postperovskite-type Fe(2)O(3) and implications for planetary magnetic records and deep interiors

Recent studies have shown that high pressure (P) induces the metallization of the Fe(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(2)O(3)) is an important...

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Detalhes bibliográficos
Main Authors: Shim, Sang-Heon, Bengtson, Amelia, Morgan, Dane, Sturhahn, Wolfgang, Catalli, Krystle, Zhao, Jiyong, Lerche, Michael, Prakapenka, Vitali
Formato: Artigo
Idioma:Inglês
Publicado em: National Academy of Sciences 2009
Assuntos:
Physical Sciences
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC2667032/
https://ncbi.nlm.nih.gov/pubmed/19279204
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.0808549106
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