Abstract
IT is now generally accepted that lava flows become permanently magnetized in the direction of the local geomagnetic field when they cool down through their Curie point1. Similarly, most sediments, on deposition, acquire a weak magnetic polarization2. This magnetization is thought to be due to lining-up of the minute permanently magnetized particles of the ferromagnetic minerals as they sink to the bottom. If used with caution, studies of rock magnetism may therefore yield valuable data concerning the direction of the geomagnetic field in the past.
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References
cf. Hospers, J., Nature, 168, 1111 (1951).
cf. Griffiths, D. H., Nature, 172, 539 (1953).
Chevallier, R., Ann. Phys., Ser. 10, 4, 5 (1925).
Hospers, J., Proc. Kon. Ned. Akad. Wet., B, 56, 467 (1953); 57, 112 (1954).
Johnson, E. A., Murphy, T., and Torreson, O. W., J. Terr. Mag. Atmos. Elec., 53, 349 (1948).
Bancroft, A. M., “The Magnetic Properties of Varved Clays”, M.Sc. thesis, University of Birmingham (1951).
Fisher, R. A., Proc. Roy. Soc., A, 217, 295 (1953).
Roche, A., C.R. Acad. Sci., Paris, 233, 1132 (1951).
Bruckshaw, J. McG., and Robertson, E. I., Mon. Not. Roy. Astro. Soc., Geophys. Supp., 5, 308 (1949).
Roche, A., C.R. Acad. Sci., Paris, 230, 113 (1950). and personal communication.
Vincenz, S. A. A. S., “Remanent Magnetism of Some Igneous Rocks of Great Britain”, Ph.D. thesis, University of London (1952).
Hospers, J., and Charlesworth, H. A. K., Mon. Not. Roy. Astro. Soc., Geophys. Supp. (in the press).
Bruckshaw, J. McG., Nature, 171, 500 (1953).
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HOSPERS, J. Rock Magnetism and Polar Wandering. Nature 173, 1183–1184 (1954). https://doi.org/10.1038/1731183a0
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DOI: https://doi.org/10.1038/1731183a0
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