Fig. 3
From: Direct evidence of active tectonics along the offshore sector of the Dinaric Fault System
Selected high-resolution seismic profiles from the NE Kvarner area showing the styles of neotectonic deformation affecting Quaternary sediments. Active faults are not observed near the seafloor. Note the tectonic folding and faulting of the older Quaternary strata in Unit 3 (profiles A-A’, B-B’) in response to the neotectonic movements. The location of the profiles and regional bathymetric data is given in Fig. 2.
