Quantum critical point and spin fluctuations in lower-mantle ferropericlase

Ferropericlase [(Mg,Fe)O] is one of the most abundant minerals of the earth’s lower mantle. The high-spin (HS) to low-spin (LS) transition in the Fe(2+) ions may dramatically alter the physical and chemical properties of (Mg,Fe)O in the deep mantle. To understand the effects of compression on the gr...

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Autors principals: Lyubutin, Igor S., Struzhkin, Viktor V., Mironovich, A. A., Gavriliuk, Alexander G., Naumov, Pavel G., Lin, Jung-Fu, Ovchinnikov, Sergey G., Sinogeikin, Stanislav, Chow, Paul, Xiao, Yuming, Hemley, Russell J.
Format: Artigo
Idioma:Inglês
Publicat: National Academy of Sciences 2013
Matèries:
Physical Sciences
Accés en línia:https://ncbi.nlm.nih.gov/pmc/articles/PMC3645530/
https://ncbi.nlm.nih.gov/pubmed/23589892
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1304827110
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