Abstract
Use of low temperature (LT) magnetic transitions to
identify magnetic minerals that carry a remanence – either
natural or laboratory-induced – at room temperature, is a
classic tool in rock magnetism (e.g. Nagata et al., 1964;
Kosterov, 2007). This particularly applies to magnetite
(Verwey transition at 118 K) and hematite (Morin
transition at 265 K), transitions
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