Pregled bibliografske jedinice broj: 1262398
Structural architecture and kinematic properties of faults in the Dubrovnik area and its hinterland (Croatia, Bosnia and Herzegovina, Montenegro)
Structural architecture and kinematic properties of faults in the Dubrovnik area and its hinterland (Croatia, Bosnia and Herzegovina, Montenegro) // Proceedings of the 11th International INQUA Workshop on Paleoseismology, Active Tectonics and Archaeoseismology ("PATA Days") 25 - 30 September 2022, Aix-En-Provence, FRANCE / Baize, Stéphane ; Rizza, Magali (ur.).
Aix-en-Provence, Francuska, 2023. str. 145-148 doi:10.5281/zenodo.7736477 (poster, međunarodna recenzija, cjeloviti rad (in extenso), znanstveni)
CROSBI ID: 1262398 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Structural architecture and kinematic properties
of faults in the Dubrovnik area and its hinterland
(Croatia, Bosnia and Herzegovina, Montenegro)
Autori
Maslač, Josipa ; Matoš, Bojan ; Vlahović, Igor ; Pavičić, Ivica
Vrsta, podvrsta i kategorija rada
Radovi u zbornicima skupova, cjeloviti rad (in extenso), znanstveni
Izvornik
Proceedings of the 11th International INQUA Workshop on Paleoseismology, Active Tectonics and Archaeoseismology ("PATA Days") 25 - 30 September 2022, Aix-En-Provence, FRANCE
/ Baize, Stéphane ; Rizza, Magali - , 2023, 145-148
Skup
11th International INQUA Workshop on Paleoseismology, Active Tectonics and Archaeoseismology ("PATA Days")
Mjesto i datum
Aix-en-Provence, Francuska, 25.09.2022. - 30.09.2022
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
Dinarides ; nappe tectonics ; 2D/3D structural modelling ; seismogenic source ; estimated magnitudes
Sažetak
Dalmatia is considered as one of the three tectonically most active regions in Croatia, characterized by moderate to strong seismicity with several instrumentally recorded earthquakes of Mw6. Identification of potential seismogenic sources and their detailed segmentation within epicentral areas is of great importance in seismic hazard and risk assessment procedure. Results of structural modelling with associated depths and faults geometrical relations as well as a seismological data indicate fault-related fold structure that accommodated vertical displacement more than 3500 m. Furthermore, faults geometrical peculiarities suggest complex tectonic history associated with presence of Triassic ductile deposits resulting with complex seismogenic source geometry alongside associated distribution of hypocenters. Based on the 3D modelling, empirical computations of identified fault segments maximal magnitudes are estimated in a range between Mw 6.29-7.53.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Ustanove:
Hrvatski geološki institut,
Rudarsko-geološko-naftni fakultet, Zagreb