Fig. 6From: Evaluating igneous sources of the Taveyannaz formation in the Central Alps by detrital zircon U–Pb age dating and geochemistryProbability U–Pb age curves of detrital zircon ages from sandstones of the Taveyannaz, Elm/Matt and Grés de Val d’Illiez formations. Only concordant ages are considered and also small error ellipses situated close and only below the concordant age curve (Ludwig 2009, ISOPLOT). Time scale after Gradstein et al. (2012)Back to article page