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Swiss Journal of Geosciences
Fig. 9 | Swiss Journal of Geosciences

Fig. 9

From: Middle-Late Jurassic syndepositional tectonics recorded in the Ligurian Briançonnais succession (Marguareis–Mongioie area, Ligurian Alps, NW Italy)

Fig. 9

a Structure probably related to a growth fault within the Calcari di Rio di Nava on the eastern side of the Cima della Fascia. Dotted lines mark two bedding planes within the CRN. This geometry can be interpreted as the result of a syndepositional tilt related to a normal fault, as sketched in b. The boxed area shows the area of a

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