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Geothermal Energy

Science – Society – Technology

Fig. 7 | Geothermal Energy

Fig. 7

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. 7

Seismic cross sections imaging the Rotliegend and pre-Permian at the Groß-Schönebeck site. A Locations of the profiles presented and borehole E GrSk 3/90. B, C NW–SE sections, D NNE–SSW section. The base of the Zechstein salt is evident by the dominant reflector band in all three sections (the lowermost interpreted as Z3). Mainly homogeneous internal reflections within the Rotliegend successions are prevailing (R3, R6, C1), and the Elbe reservoir sandstone (ERS) could be recognized as continuous reflection band. Several internal features occur in the pre-Rotliegend below the base of the Havel Subgroup (R6, black arrows). The red arrows mark seismic multiples

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