GNGTS 2024 - Atti del 42° Convegno Nazionale

Session 1.1 GNGTS 2024 underscores the complexity of fault identfcaton and the need for a multdisciplinary approach in understanding seismic events. Fig. 1 – Seismotectonic setngs of the study area. Solid barbed lines represent the major tectonic lineaments of the area. Orange circles are instrumental seismicity from the ESHM20 catalog (Grunthal and Whalstrom, 2012; Rovida and Antonucci, 2021); red stars are the greatest seismic events (M>6). The botom inset is a sketch map of the actve faults (Sebrier et al., 2016) and of the 2023 seismic sequence in Morocco; the box is the area of the right upper inset showing the ALOS-2 displacement map. The lef upper inset is a tectonic sketch of the western Mediterranean region. References Atzori S., Hunstad I., Chini M., Salvi S., Tolomei C., Bignami C., Stramondo S., Trasat E., Antonioli A., Boschi E.; 2009: Finite fault inversion of DInSAR coseismic displacement of the 2009 L’Aquila earthquake (Central Italy). Geophys. Res. Let., 36(15), doi:10.1029/2009GL039293.