western Anatolia (Turkey). The exploited fluids are of meteoric origin, mixed with deep
magmatic fluids, which interacted with the metamorphic rocks of the Menderes Massif. The
geothermal fluids are channeled along Quaternary faults belonging to the main normal faults
system delimiting the northern side of the Denizli Basin and their associated transfer zones.
In this study, hydrochemical and isotopic analyses of the thermal and cold waters allow us to …