Fig. 6From: From pilot knowledge via integrated reservoir characterization to utilization perspectives of deep geothermal reservoirs: the 3D model of Groß Schönebeck (North German Basin)Depth-converted seismic sections along NW–SE trending profile B (for location see Fig. 7). A Post-stack time migration without CRS stack, B pre-stack depth migration with CRS stack, C pre-stack depth migration with multiple reduction (see also Table 1). Black arrows indicate processing artefacts; the red arrow marks a multiple reflectionBack to article page