Fig. 10From: RETRACTED ARTICLE: Predictability and controlling factors of overpressure in the North Alpine Foreland Basin, SE Germany: an interdisciplinary post-drill analysis of the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 wellNon-decompacted sedimentation rates (thickness divided by time interval) for Cenozoic strata from tops of the calibration wells and the Geretsried GEN-1 well. In addition, the maximum observed pore pressure in equivalent mud weight EMWmax in g/cm3 is displayed for each wellBack to article page