Fig. 8From: Determination of the Earth’s structure based on intermediate-period surface wave recordings of tidal gravimeters: a case studyExamples of checkerboard test of the inverted model for the GWR C021 superconducting gravimeter (Membach) for three regions: Italy (a, d), Greece b, e and Western Turkey (c, f); positive/negative anomalies thicknesses equal to \(20\,\)km a–c and \(60\,\)km d–f (red/blue shaded areas) together with recovered anomalies (black solid line)Back to article page