A pulsed field technique for the study of magnetic grains in rocks

Details A pulsed field technique for the study of magnetic grains in rocks A pulsed field technique for the study of magnetic grains in rocks

Jun 1987

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1987pepi...46..259r&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 46, Issue 1-3, p. 259-262.

Physics

Scientific paper

A rapid method using pulsed magnetic fields for the measurement of basalt hysteresis parameters, both at room and liquid nitrogen temperatures, has been described. Results obtained using this method on a large number of samples indicate that the coercive force at 77 K, rather than the relative remanence, is a better parameter for delineating the composition and domain state of the magnetic grains in rocks.

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