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Co-emergence of magnetic order and structural fluctuations in magnetite

The nature of the Verwey transition occurring at T(V) ≈ 125 K in magnetite (Fe(3)O(4)) has been an outstanding problem over many decades. A complex low temperature electronic order was recently discovered and associated structural fluctuations persisting above T(V) are widely reported, but the origi...

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Bibliografske podrobnosti
izdano v:Nat Commun
Main Authors: Perversi, Giuditta, Pachoud, Elise, Cumby, James, Hudspeth, Jessica M., Wright, Jon P., Kimber, Simon A. J., Paul Attfield, J.
Format: Artigo
Jezik:Inglês
Izdano: Nature Publishing Group UK 2019
Teme:
Online dostop:https://ncbi.nlm.nih.gov/pmc/articles/PMC6599026/
https://ncbi.nlm.nih.gov/pubmed/31253806
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-019-10949-9
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