Research Article

Fault-Related Controls on Upward Hydrothermal Flow: An Integrated Geological Study of the Têt Fault System, Eastern Pyrénées (France)

Figure 3

Structural sketch of the study area (the Têt Valley), mapping the principal faults, lithologies, and hot springs with temperatures. Six principal clusters are observed, located at the bottom of the Canigou-Carança-Puigmal Ranges, along the brittle Têt fault and the CMNC Hercynian ductile fault. Some of these sites also correspond to the intersection between subsidiary brittle faults with the Têt fault. The location of Figure 4 is noted (white lines).