Fig. 5From: Geothermal resources assessment using temperature–depth relationships in the fault-controlled hydrothermal system of Aristino-Traianoupolis area, Northern Greece(a) Fractured zone across the buried segment of “fault 2” to the south and (b) Buried segments of the intersected Faults “3 and 3.1.” Both show isotherms flexure due to the upwelling of thermal waters in the form of well-oriented “heat intrusions” through fault-controlled damage zonesBack to article page