Resumen de La utilización de la anisotropía de 50 la susceptibilidad magnética (ASM) en el estudio de la deformación finita: ejemplo en la zona milonítica de Cap de Creus (Catalunya)
ABSTRACT The magnetic susceptibility anisotropy (MSA) of the Roses Granodiorite has been studied.
The magnetic fabric is due to the shear zones that affect these rocks. In this sense, the kmin axes of the MSA are paralel to the foliation pales and the kmax axes are parallel to the direction of the mineral elongation measured in the field. The Flinn-type diagram to study the ellipsoid shape indicates oblateness of the MSA ellipsoid.
