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The effects of dislocations on crystallographic twins and domain wall motion in magnetite at the Verwey transition
Pure magnetite experiences a first-order phase transition (the Verwey transition) near 120–125 K wherein the mineral’s symmetry changes from cubic to monoclinic. This transformation results in the formation of fine-scale crystallographic twins and is accompanied by a profound change in magnetic prop...
Autores principales: | , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Springer Berlin Heidelberg
2019
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6383955/ https://www.ncbi.nlm.nih.gov/pubmed/30872945 http://dx.doi.org/10.1186/s40623-018-0981-7 |