Fig. 5From: Determination of the Earth’s structure based on intermediate-period surface wave recordings of tidal gravimeters: a case studyAveraged dispersion curves of group-velocity of fundamental-mode Rayleigh waves (solid and dashed lines) with the standard deviation of individual measurements (shaded areas) and minimum and maximum value of the background model (dash-dotted grey lines) for each instrument of the Black Forest, Membach and Rochefort stations calculated for the Italy, Greece and Western Turkey regions, respectivelyBack to article page