Fig. 7From: Predictability and controlling factors of overpressure in the North Alpine Foreland Basin, SE Germany: an interdisciplinary post-drill analysis of the Geretsried GEN-1 deep geothermal wellIsopach maps of each layer of the 3D basin model, except for the Quaternary (thickness generally < 100 m) and Jurassic, which has been modeled with a constant thickness of 600 mBack to article page