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Fig. 4 | Geothermal Energy

Fig. 4

From: Evaluation of the Lund deep geothermal exploration project in the Romeleåsen Fault Zone, South Sweden: a case study

Fig. 4

Interpretation of the conventional seismic line Lnd2 crossing the DGE-1 drill site. The line displays a ca. 2000-m-thick sedimentary succession including a complex thrusted rock block overlying the crystalline basement. Scattered reflectors in the basement are interpreted to represent bodies and dykes of metabasite and dolerite. The depth conversion is based on velocity data from the VSP survey and the Full-Wave Sonic Velocity log

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