GNGTS 2016 - Atti del 35° Convegno Nazionale

146 GNGTS 2016 S essione 1.1 proved to be a necessary tool and a powerful instrument for such interdisciplinary research, allowing managing and combining large amount of geological, geophysical and territorial data. Moreover, the DEXP method ( Depth from Extreme Points , Fedi, 2007) has been employed to constrain the geometry of the seismogenic faults (dip angle). Our multiparametric approach has provided a contribution to the seismotectonic assessment of these three areas and can be effectively applied to other areas to identify outcropping and buried active faults and give a contribution to seismic hazard assessment. References Ambrosetti P., Bartolini C., Bosi C., Carraro F., Ciaranfi N., Panizza M., Papani G., Vezzani L., Zanferrari A.; 1987: Neotectonic Map of Italy (Scale 1:500.000) . C.N.R., P. F. Geodinamica. Bigi G., Cosentino D., Parotto M., Sartori R., Scandone, P.; 1992: Structural model of Italy and gravity map, scale 1:500,000 . Progetto Finalizzato Geodinamica CNR, Quad. Ric. Sci. 3, 114. Billi A., Bosi V., De Meo A.; 1997: Structural characterization of Mount Massico in the framework of the Quaternary evolution of the coastal depressions of the Garigliano and Volturno Rivers (northern Campania, Italy). Italian Journal of Quaternary Sciences 10(1), 1997, 15-26. Bonardi G., D’Argenio B., Perrone V.; 1988: Carta Geologica dell’Appennino Meridionale in scala 1:250.000 . Mem. Soc. Geol. It, 41, 1341. Fig. 1 – Map of the faults and earthquakes datasets overlapped on a medium scale MDA. Red lines: faults from geological maps and scientific studies; white lines: maxima of the MDA map; black dots: earthquakes from ISIDE catalogue; yellow squares: earthquakes from CPT11. The yellow boxes show the three studied areas.