GNGTS 2024 - Atti del 42° Convegno Nazionale

Session 1.2 GNGTS 2024 terms of shear-wave velocity values and to identfy the main seismic impedance contrasts at depth. The preliminary outcomes show signifcant diferences between the emission area and the zone afected by mud debris fow deposits. References Bombicci S.; 1873: Descrizione della mineralogia generale della Provincia di Bologna. Mem. Acc. SC. Istt. Di Bologna, vol 4, ser. 3, pp. 57-222. Calindri S.; 1781: Dizionario corografco, georgico, oritologico, storico dell’Italia. Bologna 1781-1785, Ristampa Forni 1978. Fot S., Parolai S., Albarello D. and Picozzi M.; 2011: Applicaton of surface wave methods for seismic site characterizaton. Surv Geophys, 32(6), 777–825, htps://doi.org/10.1007/ s10712-011-9134-2. Gatuso A., Italiano F., Capasso G., D’Alessandro A., Grassa F., Pisciota A.F., Romano D.; 2021: The mud volcanoes at Santa Barbara and Aragona (Sicily, Italy): a contributon to risk assessment. Nat. Hazards Earth. Syst. Sci., 21, 3407-2419, htps://doi.org/10.5194/nhess-21-3407-2021. Martnelli G. and Judd A.; 2004: Mud volcanoes of Italy. Geological Journal 39, 49-61. Mazzini A. and Etope G.; 2017: Mud volcanism: An updated review. Earth Science Reviews., Vol.168, 81-112, htps://doi.org/10.1016/j.earscirev.2017.03.001. Corresponding author: enricopaolucci83@gmail.com