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Fig. 4 | Geothermal Energy

Fig. 4

From: S-wave experiments for the exploration of a deep geothermal carbonate reservoir in the German Molasse Basin

Fig. 4

VSP record at Freiham TH-1 (for location, see Fig. 1). (Left) vertical component, (middle) radial component, (right) transverse component, after bandpass filtering and trace equalization. All components show a strong reflection at the top of the carbonate platform at ~ 1600 m bsl. The radial component shows splitting of the downgoing P-wavefield into upgoing P- and S-waves. Downgoing S-waves are visible in both the radial and the transverse components, despite the fact that a vertical vibrator was used as seismic source

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