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Figure 12 | Geothermal Energy

Figure 12

From: How do permeable fractures in the Triassic sediments of Northern Alsace characterize the top of hydrothermal convective cells? Evidence from Soultz geothermal boreholes (France)

Figure 12

North-South cross section through the Soultz site showing the fracture zones in the Soultz wells. Fracture zones are located on GPK-1 (F1 to F6), GPK-2, GPK-3, GPK-4 (Z1 to Z9), EPS-1, and 4550. Permeable zones are in red, partly sealed zones are in green and sealed zones are in blue. Vertical and horizontal scales are 1/5000.

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