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Fig. 6 | SpringerPlus

Fig. 6

From: Late-Proterozoic to Paleozoic history of the peri-Gondwana Calabria–Peloritani Terrane inferred from a review of zircon chronology

Fig. 6

Histograms and probability density curves of concordant zircon ages from garnet–biotite gneisses (a) from continental crust sliver of Pollino massif (data from Laurita et al. 2014) and high-grade metasediments of Serre (b; data from Fornelli et al. 2011a). In (b) SEM images of dated zircons from high grade metasediments (from Micheletti et al. 2008) are shown (scale bar 50 μm)

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