Gyroremanent magnetization in a weakly anisotropic rock sample

Details Gyroremanent magnetization in a weakly anisotropic rock sample Gyroremanent magnetization in a weakly anisotropic rock sample

Apr 1981

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1981pepi...25..163s&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 25, Issue 2, p. 163-166.

Physics

9

Scientific paper

Gyroremanent magnetization (GRM) has been detected in a rock sample
which, from initial susceptibility measurements, is only weakly
anisotropic (⋍ 1%). In accordance with theory the GRM is
independent of the frequency of the alternating field for frequencies of
50 and 274 Hz.

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