GNGTS 2023 - Atti del 41° Convegno Nazionale

Session 3.2 ___ GNGTS 2023 Figure 3. a) Alpine Adda valley, in the proximity of Teglio (Sondrio). b) Depth migrated section at Teglio. The deep white line marks the bedrock, according to the authors of the survey. The shallower white lines mark other deposits (De Franco et al., 2009). c) Displacement amplitude spectra across the basin at its center. Note The present study has been accepted for publication in Bulletin of the Seismological Society of America on November 11th, 2022. References Bard P.Y. and Bouchon M.; 1980a: The seismic response of sediment-filled valleys. Part I. The case of incident SH waves . Bull. Seism. Soc. Am., 70, 1263-1286. Bard P.Y. and Bouchon M.; 1980b: The seismic response of sediment-filled valleys. Part II. The case of incident P and SV waves . Bull. Seism. Soc. Am., 70, 1921-1941.