GNGTS 2021 - Atti del 39° Convegno Nazionale

GNGTS 2021 S essione 3.2 482 measurements, as water temperature and chemical composition, may contribute to distinguish the different fluid components (gas, groundwater, low enthalpy salty water) that are known to occur within the shallow and deep sedimentary units. Ackowledgements Our work was supported by the National Institute of Oceanography and Applied Geophysics – OGS in the framework of the project “ Geological and tectonic evolution of the Gulf of Trieste (N-Adriatic) ”, coordinated by Martina Busetti. References Claerbout J.; 1997: T squared . Stanford Exploration Project, http://sepwww.stanford.edu/sep/prof/iei/ dspr/paper_html/node6.html. Petronio L., Lipizer M., De Santis L., Rintoul S., Wardell N.; 2009: Seismic reflections within the sea water column in the Southern Ocean, Antarctica . EAGE Annual Meeting, cp-127-00330. Petronio L., Lipizer M., De Santis L., Rintoul S., Wardell N.; 2010: Offshore seismic reflection data: an oceanographic perspective . Bollettino di Geofisica Teorica ed Applicata, 51 , 89-98. Vesnaver A., Busetti M., Baradello L.; 2021: Chirp data processing for fluid flow detection at the Gulf of Trieste (northern Adriatic Sea) . Bollettino di Geofisica Teorica ed Applicata ( in press ). Corresponding author: avesnaver@inogs.it