THE LOW TEMPERATURE TRANSITION IN MONOCLINIC PYRRHOTITE
Résumé
It is confirmed by new magnetization measurements that a magnetic transition occurs sharply at 30 K in the monoclinic pyrrhotite Fe7S8. Though its nature is not yet fully understood, this transition shows some similarities with the Verwey transition and can provide a powerful tool for the identification of pyrrhotite in rocks.
Domaines
Articles anciens
Origine : Accord explicite pour ce dépôt
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