Abstract
WHEN non-axially magnetized cylindrical specimens of a quartz-dolerite have been axially compressed in an axial magnetic field of the order of the Earth's, their natural remanent magnetism vectors have changed towards the ambient field direction.
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Creer, K. M., Irving, E., and Nairn, A. E. M., Geophys. J., 2, 319 (1959).
Graham, J. W., Buddington, A. F., and Balsey, J. R., Nature, 183, 1318 (1959).
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POWELL, D. Stress-Dependent Magnetization in Some Quartz-Dolerites. Nature 187, 225 (1960). https://doi.org/10.1038/187225a0
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DOI: https://doi.org/10.1038/187225a0
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