Quantification of recent movement potentials in Schleswig-Holstein (Germany) by GIS-based calculation of correlation coefficients

In order to investigate connections between deep tectonic and halokinetic structures and the development of recent topography, GIS-based calculation of correlation coefficients was carried out between different stratigraphic horizons of the deep Northwest German Basin (NGB) according to the Geotektonischer Atlas von NW-Deutschland'' and surface topography of Schleswig-Holstein. The results show seven areas of high correlation that are traceable from the Base Zechstein up to the recent surface topography. Five areas with high correlation are connected to NNE - SSW trending salt structures within the Gluckstadt Trough, i.e. the area of the salt domes Oldensworth, Tellingstedt, Eisendorf and, to the north of Hamburg, the area of the salt domes Elmshorn and Sievershutten. Two areas, however, with NW - SE trending high correlation are located in the northwest ( restricted to the Westschleswig Block) and the northeast ( south of Fehmarn) outside the Gluckstadt Trough. These NW - SE trending correlation areas are not related to known salt structures and/or faults but match the general orientation of faults in the NGB.