![]() ![]() This paper demonstrates results of focused multidisciplinary research, from surface geological mapping and offshore shallow seismic surveys to earthquake focal mechanisms, as an active fault identification and parametrization kit, with a final goal to produce an across-methodological integrated model of the identified features in the future. 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.2University of Zagreb, Faculty of Science, Zagreb, Croatia.1Croatian Geological Survey, Zagreb, Croatia.Tvrtko Korbar 1 *, Snježana Markušić 2, Ozren Hasan 1, Ladislav Fuček 1, Dea Brunović 1, Nikola Belić 1, Damir Palenik 1 and Vanja Kastelic 3 ![]()
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