Fig. 7From: Pliocene to Quaternary deformation in the Var Basin (Nice, SE France) and its interpretation in terms of “slow-active” faultingLocations of measured faults and corresponding stereonets (1–17). A, B and C are computations of main deformation axes by the ‘Diedres Droits’ method of Arthaud (1969) using all the measured faults in each of the A–B–C zones on the map (red compressional and blue extensional)Back to article page