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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...
| Autores principales: | , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2019
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| Materias: | |
| 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 |