GNGTS 2024 - Atti del 42° Convegno Nazionale

Session 1.1 GNGTS 2024 indicates that the simulated coseismic and cumulatve vertcal displacement felds agree with the historical observaton of the slip along the fault planes and with actual height of the morphological scarps, respectvely. Considering the lack of seismic profles onshore, the proposed model can represent an important startng point for seismotectonic modelling. Figure 3: a) Map view of the 3D model of SRF and CF, fault planes are coloured in functon of the Slip tendency (Ts). b) Confning stress state resolved at 10 km of depth. c) Vertcal displacement (dz) computed for 3 m of uniform slip on the fault planes. Black and yellow dashed lines show the mesoseismal areas for the shocks of the 1783 seismic (see also Barata, 1901; Jacques et al., 2001 for further informaton). d) Vertcal displacement (dz) computed for Tmax values of 664 m and 697 m. e) Coseismic dz profle across CF and SRF. f) Cumulatve dz profle across CF and SRF.