Periodico di Mineralogia (2015), 84, 3B (Special Issue), 657-699 DOI: 10.2451/2015PM0455 An International Journal of PERIODICO di MINERALOGIA MINERALOGY, CRYSTALLOGRAPHY, GEOCHEMISTRY, established in 1930 ORE DEPOSITS, PETROLOGY, VOLCANOLOGY and applied topics on Environment, Archaeometry and Cultural Heritage Continental collision from two perspectives: a review of Variscan metamorphism and deformation in northern Sardinia Gabriele Cruciani1,*, Chiara Montomoli2, Rodolfo Carosi3, Marcello Franceschelli1 and Mariano Puxeddu4 1 Dipartimento di Scienze Chimiche e Geologiche, Via Trentino, 51, 09127 Cagliari, Italy 2 Dipartimento di Scienze della Terra, V. S. Maria, 53, 56126 Pisa, Italy 3 Dipartimento di Scienze della Terra, V. V. Caluso, 35, 10125 Torino, Italy 4 Former researcher of the Istituto di Geoscienze e Georisorse CNR-Pisa, Via Moruzzi, 1, 56124 Pisa, Italy * Corresponding Author:
[email protected] Abstract Structural, petrological and geochronological data from the Variscan chain of northern Sardinia are discussed, with the aim to improve our knowledge on the tectono-metamorphic evolution of the northern Sardinian basement and its role in the tectonic puzzle of the southern Variscan massifs. In northern Sardinia, which corresponds to the Inner zone of the chain, the metamorphic grade rapidly increases towards the NE from biotite to sillimanite+K-feldspar zone. The highest grade rocks cropping out in the Migmatite zone reached amphibolite facies conditions in the sedimentary and igneous-derived migmatite and eclogite/granulite facies in the enclosed metabasite lenses. Evidence of HP metamorphism has also recently been found more to the south in micaschist from the garnet zone. The D1 deformation can be observed in the southern part of the Inner zone, whereas, moving progressively northwards, the D2 deformation progressively obliterates the previous foliation.