Fig. 19From: Geothermal resources assessment using temperature–depth relationships in the fault-controlled hydrothermal system of Aristino-Traianoupolis area, Northern GreeceGeneralized geological sketch (not to scale) and conceptualization of the dominant heat transfer process in the AGF. The water movement is conducted through permeable intersected faults damage zones and permeable overlapping lateral reservoirs (modified from Liotta et al. 2021)Back to article page