High temperature measurement of the saturation magnetisation for VER98-1-1

Francois Demory, Hedi Oberhänsli, Norbert Nowaczyk, Matthias Gottschalk, Richard Wirth & Rudolf Naumann
It shows a loss of a part of the signal at temperatures between 350 and 400 °C, typical disintegration temperatures for greigite. The remaining signal disappears above a temperature of 590 °C, typical for magnetite.
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