Untersuchungen zur quartären Bruchtektonik der Niederrheinischen Bucht

Ludwig Ahorner
Extensive investigations in field geology and geomorphology as well as the interpretation of numerous bore hole profiles (with occassional application of sediment-petrological methods) supported a revision of Quaternary structural activity („fortlebende Tektonik") in the Lower Rhine Valley. The stratigraphic position of the Pleistocene deposits in the western region of the Lower Rhine Valley — in particular those of the older river terraces of Rhein and Meuse — has been discussed in detail. Kind and dimension...