Figure 9From: How do permeable fractures in the Triassic sediments of Northern Alsace characterize the top of hydrothermal convective cells? Evidence from Soultz geothermal boreholes (France) Detailed BHTV image at 1,204-m depth in the well EPS-1. The BHTV shows a fracture oriented N-S and dipping westward (data from DMT-Institute for Geophysics, Germany).Back to article page