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.