Fig. 7From: Determination of the Earth’s structure based on intermediate-period surface wave recordings of tidal gravimeters: a case studyResolution matrices of the inversion scheme for the GWR C021 superconducting gravimeter and CMG3T broadband seismometer (Membach) for three regions: Italy, Greece and Western Turkey. The maximum resolution depth is marked with a black star and the optimum resolution depth with a red starBack to article page