Fig.11. Local gravity anomalies at different depths separated by interpolation cutting are compared with seismic structures a—bouguer gravity anomaly; b—gravity anomaly at depths of 200~600 m; c—gravity anomaly at depths of 600~1 000 m; d—gravity anomaly at depths of 1 000~1 400 m; e—gravity anomaly at depths of 1 400~1 800 m; f—gravity anomaly at depths of 1 800~2 200 m; g—gravity anomaly at depths of 2 200~2 600 m