Fig. 7From: 3-D seismic exploration across the deep geothermal research platform Groß Schönebeck north of Berlin/GermanyComposite of the seismic volume (migrated, depth) with selected horizons (view towards north). They exemplify the rather transparent upper Tertiary sediments (K2), the continuous internal Zechstein structure (X3), and the lowermost interpretable Rotliegend horizon (R8). The vertical sections are blended with the drilling paths, used for well tie and synthetics (cf., Fig. 2) to calibrate the reflectors. Several reflectors can be traced with high confidence across the volume, exceeding former interpretations (reflector nomenclature according to Reinhardt 1993)Back to article page