A model for the orientation process of ferromagnetic minerals in slates

Details A model for the orientation process of ferromagnetic minerals in slates A model for the orientation process of ferromagnetic minerals in slates

Nov 1976

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1976e%26psl..33..107h&link_type=abstract

Earth and Planetary Science Letters, Volume 33, Issue 1, p. 107-110.

Computer Science

1

Scientific paper

The orientation mechanism of ferromagnetic mineral grains in deforming slates (strain response model) was studied on the basis of a comparison of the degrees of magnetic anisotropy in natural slates with those calculated for the ``line/plane'' and ``passive'' models. Ferromagnetic grains reorientate mostly as rigid particles in a ductile matrix, although the possibility of a subordinate change in shape cannot be excluded.

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