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• W45243364 abstract "In attempting to read the geomagnetic record in rocks, sensitive techniques have been developed to examine the natural remanent magnetization which they carry. Research into the apparently simple and well-known technique of alternating field demagnetization has led to a fundamental discovery in the field of particle magnetism namely a remanence of gyromagnetic origin. This phenomenon can now be used to estimate rapidly the size of magnetite or maghemite particles and to detect preferential alignments of dispersed non-spherical particles in anisotropic rocks. Investigation of the deflection of the thermoremanent magnetization vector away from the local geomagnetic field vector by such anisotropic igneous rocks with the aim of being able to correct for the effect has led to yet another method of determining particle size and domain state. It has also been found that isotropic distributions of particles can be made magnetically anisotropic after they have been subjected to strong alternating or direct fields and that this effect is also particle-size dependent." @default.
• W45243364 created "2016-06-24" @default.
• W45243364 creator A5013350442 @default.
• W45243364 date "1992-01-01" @default.
• W45243364 modified "2023-09-23" @default.
• W45243364 title "Some aspects of the properties of fine particles in geomagnetism" @default.
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• W45243364 doi "https://doi.org/10.1016/b978-0-444-89552-3.50041-4" @default.
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