“…Anisotropy of the magnetic susceptibility is today a standard technique for petrofabric studies in granitoids (e.g. Archanjo et al, 1995Archanjo et al, , 2002Ferré and Améglio, 2000;McNulty et al, 2000;Neves et al, 2003;Zák et al, 2005;D'Eramo et al, 2006;Stevenson et al, 2007; and many others), having outstanding relevance in determination of magmatic lineations, which are hard to measure in the field or in the laboratory using the microscope (Bouchez et al, 1981).…”