GNGTS 2019 - Atti del 38° Convegno Nazionale

158 GNGTS 2019 S essione 1.2 Tripodi et al. , 2013; Brutto et al. , 2016). Several authors identify a partial or total detachment of the ionian slab, starting from the middle Pleistocene which induces a general uplift whose lifting rates range from 0.5 to 1.2 mm/year in 1-0.7 million of years (Monaco et al. , 1996, Wortel and Spakman, 2000; Dumas and Raffi, 2004). Materials and methods. The studies aimed at defining the seismic hazard of a territory are based on three primary sources: historical seismicity, geological information and instrumental seismic catalogs. In the present work a first study based on the comparison between instrumental Fig.1 - Study area location (modified by Tripodi et al. 2018). Fig.2 - Main recent tectonic structures (modified by Tripodi et al. 2018).