CORDIS Project
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This research investigates the magnetic properties of deep crustal materials, focusing on natural oxides that retain stable magnetic remanence at high temperatures. The project aims to enhance understanding of crustal anomalies through high-pressure experiments and advanced imaging techniques.
Magnetic anomalies from deep sources are commonly thought to be induced by the present Earth's field to magnetite bearing rocks.
Such magnetism is limited by the Curie isotherm of magnetite related to the local thermal gradient.
The proposed research challenges this picture and is important for understanding large scale crustal anomalies.
Natural rhombohedral oxides of the Fe2O3-FeTiO3 solid solution series with fine-scale exsolution intergrowths can retain a strong and very stable magnetic rema…
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