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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Detalles Bibliográficos
Autores principales: Perversi, Giuditta, Pachoud, Elise, Cumby, James, Hudspeth, Jessica M., Wright, Jon P., Kimber, Simon A. J., Paul Attfield, J.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6599026/
https://www.ncbi.nlm.nih.gov/pubmed/31253806
http://dx.doi.org/10.1038/s41467-019-10949-9

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6599026/
https://www.ncbi.nlm.nih.gov/pubmed/31253806
http://dx.doi.org/10.1038/s41467-019-10949-9

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