GNGTS 2023 - Atti del 41° Convegno Nazionale

Session 1.2 GNGTS 2023 The analysis of these signals allows the location of respective sources that appear local (tens of meters away from instruments) and shallow (within 20 m from the surface). If these emissions were actually associated with gas bubbling, this kind of outcome could represent an effective tool for measuring gas outflow and monitoring outgoing mud volcanoes activity. Bibliography Bonini M.; 2008: Elliptical mud volcano caldera as stress indicator in an active compressional setting (Nirano, Pede-Apennine margin, northern Italy) . Geology, 36(2), 131–134. Lupi M., Suski Ricci B., Kenkel J., Ricci T., Fuchs F., A. Miller S., Kemna A.; 2016: Subsurface fluid distribution and possible seismic precursory signal at the Salse di Nirano mud volcanic field, Italy . Geophysical Journal International 204: 907-917. Albachiara Brindisi: albachiara.brindi@student.unisi.it