Fig. 8From: Late-Proterozoic to Paleozoic history of the peri-Gondwana Calabria–Peloritani Terrane inferred from a review of zircon chronologyHistograms and probability density curves of inherited zircon ages in the range 1000–3400 Ma collected in the augen gneisses from Castagna (a) and Aspromonte–Peloritani (b) Units (data from Micheletti et al. 2007; Fiannacca et al. 2013)Back to article page