Zum Bau des Bersenbrücker Lobus im Stauchmoränenzug der Rehburger Phase

H. G. Wunderlich
Serial drillings in different parts of the Bersenbrück Uplands northwest of Osnabrück (Western Germany) as well as in its northern and southern reaches offer an insight into the inner structures of the zone of thrusting due to glazial overriding. These details are also laid bare even where boulder sand and sandy loess cover the schuppen-structures involving Oligocene and Miocene clays and sands as well as pre-Saalian terrace-gravels and sands.