Fig. 5From: Triassic magmatism on the transition from Variscan to Alpine cycles: evidence from U–Pb, Hf, and geochemistry of detrital mineralsHf-isotope systematics of Permian and Triassic detrital zircons, showing εHf(t) versus 206Pb/238U crystallization ages in Ma: 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