Fig. 13From: On the geothermal potential of crustal fault zones: a case study from the Pontgibaud area (French Massif Central, France)Maps of temperatures (a), permeabilities (b), isotherms (c), and thermal anomalies (d) of the Pontgibaud region (at time t0 + 15,000 years). In accordance with Fig. 11, color of boxes contours correspond to one convective regime: blues boxes correspond to areas of unicellular weak-type convection zone, oranges boxes correspond to unicellular medium-type convection zone, and reds boxes correspond to bicellular strong-type convection zoneBack to article page