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Anomalies in vertical displacement rates related to recent geodynamics were determined between Rate~e and Ljubljana by comparing leveling line data with topography of the Sava river longitudinal profile. Beside the general trend showing increase of vertical displacement in the S-N direction, segmentation of the area is noted. The later suggests that active geological structures exist in the northern part of the Ljubljana basin and in the Upper Sava valley respectively.

Identification of potentially active structures along the Sava river using topographic, and leveling line data