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Geothermal Energy

Science – Society – Technology

Fig. 9 | Geothermal Energy

Fig. 9

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. 9

Seismic attribute analysis applied for fault detection at the top (X3 horizon) and base (Z3 horizon) of Zechstein. Left column: variance along interpreted horizons based on CRS volume in time (A X3, C Z3). Right column: maximum amplitude based on CRS volume in depth (B X3, D Z3). The graben-like structure within the Leine anhydrite (X3, A, B) is clearly visible, while fault signatures are nearly absent at the base of the Zechstein (Z3, C, D). The cross marks the Groß Schönebeck drill site (E GrSk 3/90)

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