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Geothermal Energy

Science – Society – Technology

Fig. 13 | Geothermal Energy

Fig. 13

From: Porosity estimation of a geothermal carbonate reservoir in the German Molasse Basin based on seismic amplitude inversion

Fig. 13

Porosity histograms of the reservoir zone for the entire model and along the drilling paths derived from the inversion results. The wide range of porosity values results from the strong heterogeneity of the carbonates due to effect of different processes on the pore space, such as dolomitization, cementation and dissolution. Overall, the dolomitic limestone shows the highest porosities and the calcareous dolomite the lowest

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