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Fig. 6 | Swiss Journal of Geosciences

Fig. 6

From: Pliocene to Quaternary deformation in the Var Basin (Nice, SE France) and its interpretation in terms of “slow-active” faulting

Fig. 6

Field photographs of faulted and tilted Var Basin Pliocene molasse-type sediments. a Photo representative of the most common fault deformation feature in studied area, showing a striated fault plane with sinistral sense of motion in Donaréo valley. b Verticalized Pliocene strata along the St Blaise-Aspremont Fault (at ‘La Loubière’, west of Mont Cima, Fig. 4a)

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