Rinnen an der Basis des glaziaren Pleistozans in Schleswig- Holstein.

Abstract

Using well data the pre Quaternary subcrop and the base of glacial Pleistocene are mapped. Their configuration is rather independent of halokinetinally induced troughs and salt structures. Channels in diverse directions were formed rather quickly by exaration, glacial tectonic and subglacial erosion. For many channels an Elster age can be proved.-from English summary