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Hydrochemical characteristics of thermal waters in Middle Kur depression structures

The distribution of thermal waters in the structures of Middle Kur depression is different. Thus, Barda, Terter and Aghjabedi studied structures are characterized with the highest water inflow. The water temperature reaches up to 50 оС in the flow. Chloride-natrium methane waters are distributed here predominantly. The migration of thermal waters is largely effected by thermo-lift and gas factor. The most prospective water-bearing complexes are the Cretaceous and Miocene (Maikop, Chokrak) sediments. According to the results of technical-economic feasibilities (temporary and permanent conditions) of Barda, Terter and Aghjabedi studied areas the thermal waters from Maikop horizon have healing properties. It is necessary to enhance the further research surveys on these areas of Middle Kur depression.