Fig. 10From: Middle-Late Jurassic syndepositional tectonics recorded in the Ligurian Briançonnais succession (Marguareis–Mongioie area, Ligurian Alps, NW Italy)Neptunian dikes. Complex pattern of fissures within the Calcari di Rio di Nava in the Piano Ambrogi area. Two sets of fractures with different infillings and crosscutting one another are clearly recognizable (red infilling large arrow; yellow infilling small arrows). Camera lens cap for scale is 4 cm in diameterBack to article page