Fig. 4From: Late-Proterozoic to Paleozoic history of the peri-Gondwana Calabria–Peloritani Terrane inferred from a review of zircon chronologyHistograms and probability density curves of concordant zircon ages from augen gneisses of Aspromonte–Peloritani (a) and Castagna Units (b) are reported (data from Fiannacca et al. 2013; Micheletti et al. 2007)Back to article page