Abstract
Summary. Recent experimental work by Edwards has demonstrated that rotational remanent magnetization (RRM) is not a maximum when the alternating field is normal to the rotation axis of the sample (a rock) but is greatest when the angle is about 75°. Experiments involving the production of ARM during sample rotation gave a similar result with a maximum at about 60°. These results are explained here in terms of the response of an isotropic assembly of identical single‐domain particles to a strong alternating magnetic field. Copyright © 1985, Wiley Blackwell. All rights reserved
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Stephenson, A. (1985). The angular dependence of rotational and anhysteretic remanent magnetizations in rotating rock samples. Geophysical Journal of the Royal Astronomical Society, 83(3), 787–796. https://doi.org/10.1111/j.1365-246X.1985.tb04338.x
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