Fig. 12From: Pliocene to Quaternary deformation in the Var Basin (Nice, SE France) and its interpretation in terms of “slow-active” faulting Rose diagrams of striation directions of measured strained pebbles, shown by locality. Note that the striation directions are mainly controlled by the main fault direction (N20oE–N30°E along the Donareo Fault and N150°E–N0° along the St Blaise Aspremont Fault), which is globally compatible with N–S shorteningBack to article page