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Geothermal Energy

Science – Society – Technology

Fig. 17 | Geothermal Energy

Fig. 17

From: From pilot knowledge via integrated reservoir characterization to utilization perspectives of deep geothermal reservoirs: the 3D model of Groß Schönebeck (North German Basin)

Fig. 17

Thickness maps of the Quaternary deposits (A) and of the Tertiary Rupelton (B) based on Stackebrandt and Manhenke (2010). Superimposed in grey lines are the mapped main faults in the upper Zechstein (this study) and the orientation of the seismic profile shown in C. C Seismic section of the pre-stack depth migration volume with CRS stack after depthing (profile D in Fig. 6) showing less continuity of seismic reflectors in the stippled area

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