Abstract
Complex endogenous geotectonic processes predisposed the Spreca fault zone with different geotectonic structures, within which an aquifer of thermomineral waters with CO2 escalation was formed, in the Gracanica area, located in the lower Spreca depression, which makes contact with two different rock complexes: volcanogenic-sedimentary and ultramafic of the "central ophiolitic mélange" complex south of the Spreca fault zone and the Cretaceous-Tertiary complex of sediments "internal ophiolitic tectonized mélange" north of the fault zone. Key words: Spreca fault, thermo-mineral water, borehole, temperature
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