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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...

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Detalles Bibliográficos
Autores principales: Lindquist, Anna K., Feinberg, Joshua M., Harrison, Richard J., Loudon, James C., Newell, Andrew J.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer Berlin Heidelberg 2019
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