GNGTS 2024 - Atti del 42° Convegno Nazionale

Session 1.1 GNGTS 2024 3D model architecture The database of the seismotectonic model (Fig. 1) is organized in three levels: i) The frst level consists of folders and subfolders containing 2D input data imported into the sofware Leapfrog Works, version 2023.2. The georeferenced data are: eight new geological cross-sectons deriving from detailed feldwork carried out along the Pedeapenninic margin; six diferent cross sectons from the two seismotectonic maps of the Emilia-Romagna region (Boccalet et al., 2004; Martelli et al., 2016); twenty-three geological cross sectons from the CARG project (Martelli et al., 2009; Gasperi et al., 2005; Panini et al., 2002; Betelli et al., 2002; Pizziolo et al., 2002; Cerrina Feroni et al., 2002; Plesi et al., 2002); 113 boreholes and eighteen deep seismic lines from the ViDePi project ( htps://www.videpi.com/videpi/ videpi.asp ); hypocenters from > 8000 seismic events extracted from the natonal catalogs (ISIDe Working Group, 2007; Rovida et al., 2020, 2022) and seventy-nine focal mechanisms from Martelli et al. (2016); ii) The second level stores 3D geometries created directly within the model from the above input data, such as polylines and meshes; iii) The third level contains the seismotectonic model with eight reconstructed chronostratgraphic units and ffy-seven mapped actve faults.