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Geothermal Energy

Science – Society – Technology

Fig. 7 | Geothermal Energy

Fig. 7

From: Predictability of properties of a fractured geothermal reservoir: the opportunities and limitations of an outcrop analogue study

Fig. 7

Fracture orientation and intensity in Cleebourg, shown for three individual layers. In layers 1 and 2, the fracture orientations are comparable and the fracture intensity increases towards the fault core. In layer 3, fracture orientation and intensity show a different pattern. Rose diagrams with equal area scaling and 10° bin size and equal area pole point plots on the lower hemisphere

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