“…This recognized structural control motivated geologists to improve their knowledge about the geometry and timing of different plutons in relation to major orogenic events. Work has included detailed structural maps of Variscan batholiths that have been coupled to high-resolution geochronological studies in the French Massif Central (Faure, Cocherie, Mézème, Charles, & Rossi, 2010;Gébelin et al, 2009), External Crystalline Massifs on the western Alps (Rubatto, Ferrando, Compagnoni, & Lombardo, 2010), the Pyrenean region (Liesa et al, 2011;Vilà et al, 2010) and the Corsica-Sardinia block (Casini, Cuccuru, Maino, Oggiano, & Tiepolo, 2012;Gattacceca et al, 2004;Gébelin et al, 2009;Rossi & Cocherie, 1991). However, recent work on the Sardinian part of the Corsica-Sardinia Batholith have focused on petrological aspects related to the origin of melts (Cruciani, Franceschelli, Jung, Puxeddu, & Utzeri, 2008;Ferré & Leake, 2001;Gaggero, Oggiano, Buzzi, Slejko, & Cortesogno, 2007;Macera, Di Pisa, & Gasperini, 2011).…”