Annealing natural olivine up to 1500°C produces phase changes detectable by 4-polarized IR reflectance and induces magnetization via precipitation of Fe-rich oxides.
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Olivine annealed up to 1500 C: changes traced by polarised IR reflectance and magnetization
Annealing natural olivine up to 1500°C produces phase changes detectable by 4-polarized IR reflectance and induces magnetization via precipitation of Fe-rich oxides.