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

Figure 8

Ductile fault outcrops and thin sections. (a) Vernet-les-Bains mylonitic outcrop with foliation parallel dissolution cavities. (b) Vernet-les-Bains gneiss thin section showing a hole (Ho) parallel to the foliation crosscutting a carbonate vein (Cv). Oxides and chlorite (Ox + Chl) localize along the foliation. (c) Dissolution cavities along the fractured gneissic foliation at Canaveilles hot springs. Doted white line surround mineral deposit.

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(b)

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