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Description
Ferromagnetic minerals such as magnetite carry a remanent magnetization only at temperatures below the Curie Point, but at higher temperatures they are paramagnetic. In a volcanic rock and when cooling below the Curie Point, crystals acquire a remanent magnetization that is anti-parallel to the magnetic field at its location. This magnetization is called thermoremanent magnetization. |
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Keywords remanent magnetization, thermoremanent magnetization, Curie temperature |
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Copyright Owner Enduring Resources for Earth Science Education (ERESE) |
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