Magnetic fabrics and superimposed deformations: example of Dalradian rocks from the southwest Highlands of Scotland

Details Magnetic fabrics and superimposed deformations: example of Dalradian rocks from the southwest Highlands of Scotland Magnetic fabrics and superimposed deformations: example of Dalradian rocks from the southwest Highlands of Scotland

Nov 1985

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1985pepi...40..187h&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 40, Issue 3, p. 187-200.

Physics

6

Scientific paper

Analysis of anisotropy differences in specimens close in the same sample permits the separation of anisotropies due to ferrimagnetic minerals and their dia-paramagnetic matrix. This method, previously described, has been applied to rocks, affected by superimposed deformations, from the Dalradian of Scotland. It appears that ferrimagnetics anisotropy is often found in relation with the secondary deformation, even though matrix anisotropy is related to the primary deformation. This last anisotropy has here a dominant effect on the orientation of the resultant fabric of the whole rock.

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