Magnetic domains and magnetic stability of cohenite from the Morasko iron meteorite
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文摘
Magnetic domain structure of cohenite from the Morasko iron meteorite was investigated by Bitter pattern method, magneto-optical imaging and magnetic force microscopy. Strong magnetocrystalline anisotropy explains high magnetic stability. Magnetic domain structure shows high sensitivity to local microstructural heterogeneities. Cohenite is probably a good recorder of magnetic fields in planetary core material.

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