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Swiss Journal of Geosciences
Fig. 2 | Swiss Journal of Geosciences

Fig. 2

From: The Teggiolo zone: a key to the Helvetic–Penninic connection (stratigraphy and tectonics in the Val Bavona, Ticino, Central Alps)

Fig. 2

Synthetic stratigraphic sections of the Teggiolo zone in the Val Bavona. The sedimentary cycles distinguished in the text are as follows: first cycle, Dolomite (Triassic); second cycle, Ri d’Antabia conglomerate, Sevinèra sandstone, Sevinèra marble, Vanis banded marble (Jurassic–Early Cretaceous); third cycle, Piano delle Creste sandstone, Mèdola quartzite (Late Cretaceous–Tertiary); fourth cycle, Robièi wildflysch (Tertiary)

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