Figure 11From: How do permeable fractures in the Triassic sediments of Northern Alsace characterize the top of hydrothermal convective cells? Evidence from Soultz geothermal boreholes (France) Equilibrium temperature profile from 0- to 1,500-m depth in the well 4550. The equilibrium temperature profile was obtained several months after drilling operation was finished (data from LIAG-Hannover, Germany).Back to article page