Table S3. Ground seismic parameters estimated at the different seismic station locations based on active seismic surveys. \(v_{p0}\) is the phase velocity of the Raleigh wave at a frequency \(f_{0}\) = 1 Hz and \(\xi\) [-] a dimensionless exponent used to scale a frequency-dependent decay in seismic signal (equations [1a] and [1b] in the main manuscript). \(K_{0}\) is a dimensionless quality factor at a frequency \(f_{0}\) = 1 Hz and \(\eta\) [-] a dimensionless exponent that expresses the change in the quality factor K with frequency (equation [1c] in the main manuscript). Note that a single active seismic experiment encompassing multiple sensors has been performed for the group S10/S12, S16/S20 and S22/23/24 thanks to their geographical proximity.