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Figure 8 | Geothermal Energy

Figure 8

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 8

Synthetic log of GPK-1. The synthetic log shows lithology, mud losses, GR, neutron porosity (NPHI), bulk density (RHOB), calipers (CAL1 and CAL2), and temperature data (Temp87). Fracture zones are indicated: F1 to F6. Permeable zones are in red and partly sealed zones are in green. Depths are expressed in measured depth.

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