Ferromagnetic resonance characterization of greigite (Fe 3 S 4 ), monoclinic pyrrhotite (Fe 7 S 8 ), and non-interacting titanomagnetite (Fe 3-x Ti x O 4 )
Ferromagnetic resonance (FMR) spectroscopy has become an increasingly useful tool for studying the magnetic properties of natural samples. Magnetite (Fe 3O 4) is the only magnetic mineral that has been well characterized using FMR. This limits the wider use of FMR in rock magnetism and paleomagnetism. In this study, we applied FMR analysis to a range of magnetic minerals, including greigite (Fe 3S 4), monoclinic pyrrhotite (Fe 7S 8), magnetically non-interacting titanomagnetite (Fe 3-xTi xO 4),...[Show more]
|Collections||ANU Research Publications|
|Source:||Geochemistry, Geophysics, Geosystems. G3|
|01_Chang_Ferromagnetic_resonance_2012.pdf||998.41 kB||Adobe PDF|
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