![]() Moreover, anthropogenic modifications greatly complicate access to the surface geological and geomorphological data. In the Kvarner region of the External Dinarides, an area with low-to-moderate seismicity related to the Adriatic microplate (Adria) northward movement, we deal with faults in predominantly carbonate rocks within tectonically complex NW-SE striking fold-and-thrust belt, which makes the identification and parametrization of the active structures challenging. 3Istituto Nazionale di Geofisica e Vulcanologia (INGV), L’Aquila, ItalyĪctive tectonics in long-lived orogenic belts usually manifests on the preexisting inherited structures. ![]()
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