GNGTS 2024 - Atti del 42° Convegno Nazionale

Session 3.2 GNGTS 2024 Fig. 3 - Sub-botom profle originally stored in envelope mode(a) and below a zoom pseudo-seismic secton(b) (Baradello et al. 2021) near the sediment core NW31 projecton onto the profle. References Baradello L (2014) An improved processing sequence for uncorrelated Chirp sonar data. Marine Geophys Res 35(4):337–344 Baradello L., Bataglia F., Vesnaver A. (2021) Fast method to transform chirp envelope data into pseudo-seismic data. Marine Geophys Res 42:14 htps://doi.org/10.1007/s11001-021-09436-y Henkart P (2006) Chirp Sub-Botom profler processing – a review. Sea Technol 47(10):35–38 Quinn R, Bull JM, Dix JK (1998) Optmal processing of marine high resoluton seismic refecton (Chirp) data. Marine Geophys Res. 20:13–20 Corresponding author: csauli@ogs.it