Fig. 9From: Determination of the Earth’s structure based on intermediate-period surface wave recordings of tidal gravimeters: a case studyThe coefficient of correlation of original and recovered anomalies for the GWR C021 superconducting gravimeter (Membach) for three regions: Italy (a), Greece b and Western Turkey (c), respectively. The depth range of two uppermost anomalies is marked by dashed white linesBack to article page