Fig. 4From: Triassic magmatism on the transition from Variscan to Alpine cycles: evidence from U–Pb, Hf, and geochemistry of detrital mineralsProbability density distribution of concordant detrital zircon ages (Ma). Concordia diagrams are not shown. Numbers in brackets next to the sample labels represent the number of analyses. a Eastern Alpine formations. Fuorn and Saluver formations taken from Beltrán-Triviño et al. (2013), b Southern Alps units, eastern Lombardy section; and C Southern Alps units, western Lombardy sectionBack to article page