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Fig. 4 | Swiss Journal of Geosciences

Fig. 4

From: Triassic magmatism on the transition from Variscan to Alpine cycles: evidence from U–Pb, Hf, and geochemistry of detrital minerals

Fig. 4

Probability 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 section

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