Fig. 10From: Triassic magmatism on the transition from Variscan to Alpine cycles: evidence from U–Pb, Hf, and geochemistry of detrital mineralsSketch (not to scale) of the tectonic interpretation during the Permian and Triassic magmatic events, and during the Jurassic oceanic crust formation. The stars indicate the possible position of the analysed units. The orientation of the profiles is shown in the palaeogeographic map in Fig. 2bBack to article page