GNGTS 2023 - Atti del 41° Convegno Nazionale

Session 1.2 GNGTS 2023 The Ionian Sea has a shallower Moho to the east that deepens westward toward the subduction of the Ionian slab below the Calabrian Arc, highlighted by the deep seismicity. In this work, the Ionian slab is modified with respect to the model proposed by DISS and its geometry has been adapted to the hypocenters of the deepest seismic events (>40 km deep). Therefore it was verticalized starting from about 200 km deep and between 65 km and 250 km deep was also extended laterally (Fig. 3).