Modelling the relationship between magnetic fabric and strain in polymineralic rocks

Details Modelling the relationship between magnetic fabric and strain in polymineralic rocks Modelling the relationship between magnetic fabric and strain in polymineralic rocks

Mar 1992

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992pepi...70..214h&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 70, Issue 3-4, p. 214-218.

Physics

5

Scientific paper

We present a model that is applicable to the relatively frequent case of rocks in which the magnetic fabric is dominated by uniaxial paramagnetic minerals, and in which the deformation (pure shear) corresponds to the March-Fernandez model. Borradaile et al.'s procedure for the isolation of the magnetic fabric of monocrystals of anisotropic components allows us to obtain the magnetic properties equivalent to those of all the component minerals if they should be artificially aligned. In the case of real component minerals with similar shape parameters, χ (dependent on dimension ratio), these properties will correspond to those of a theoretical equivalent mineral. Therefore, finite strain and orientation tensors may be determined from magnetic fabric measurements of such polymineralic rocks.

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