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Fig. 10 | Geothermal Energy

Fig. 10

From: RETRACTED ARTICLE: Predictability and controlling factors of overpressure in the North Alpine Foreland Basin, SE Germany: an interdisciplinary post-drill analysis of the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 well

Fig. 10

Non-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 well

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