Fig. 7
From: Late Palaeozoic tectonics in Central Mediterranean: a reappraisal
Calabria lower (a–c) and intermediate crust (d, e): a granulitic metagabbro (Curinga); b felsic granulite, garnet-sillimanite rich fels (Marina di Vibo); c Bt + Pl + Kfs + Sil + Grt ± Ms bearing migmatitic paragneiss (kinzigite Auct.); d tonalite emplaced at middle crust level and characterized by a dominant magmatic fabric (Ioppolo); e foliated peraluminous granodiorite (Parghelia)