Sources of magnetic susceptibility in a slate

Details Sources of magnetic susceptibility in a slate Sources of magnetic susceptibility in a slate

Jan 1986

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1986e%26psl..76..336b&link_type=abstract

Earth and Planetary Science Letters, Volume 76, Issue 3-4, p. 336-340.

Computer Science

30

Scientific paper

Magnetic susceptibility and its anisotropy in the Borrowdale Volcanic slates at Kentmere in the English Lake District are attributed largely to preferred orientation of a paramagnetic chlorite of diabantite-ripidolite composition. In units of 10-6 cgs/g, the principal susceptibilities for the slates are 9.61; 9.42; 8.69 and for the chlorite grains the minimum anisotropy is represented by principal susceptibilities of 11.57; 11.22 and 9.15. Because the magnetic susceptibility is carried by a tightly packed, matrix-forming mineral that has recrystallised during the deformation it is not possible to imagine simple grain rotation as being responsible for the anisotropy of susceptibility.

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