Abstract
In this study, geothermal waters of Havran were studied in detail. In the area, Karakaya formation in Early Triassic age is the basement consisting volcanic and sedimentary rocks such as of basalts, mudstones, and radiolarites in which there are intercalations of limestone, sandstones and conglomerates. Granodiorite intrusions in Oligocene to Miocene age occur in association with intense volcanic events in the area. From Upper Oligocene to Early Miocene, andesitic and dacitic pyroclastics occur due to intensively volcanism in the area. Later, lacustrine sediments consisting of conglomerates, sandstones, claystones, marls and limestones form from Middle to Upper Miocene. Geothermal waters in the area of Havran are of Na-Ca-(SO4)-HCO3, Na-(SO4)-HCO3 and Na-SO4 type. The geothermal waters display immature waters and were represented within this study as a hydrogeological model.
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