Published January 2021, Pg. 8-12

Section: Geology and geophysics

UOT: 550: 622.276 (479.24)

DOI: 10.37474/0365-8554/2021-1-8-12

Geothermic conditions of thermal waters in the structures of Middle Kur depression

S.Sh. Salahov Cand. in Geol.-Min.Sc. - National Survey of Geological Exploration, Ministry of Ecology and Natural Resources

U.S. Salahova - Azerbaijan State University of Oil and Industry

Geothermic conditions in Middle Kur depression are quite complicated. Locally and regionally, the temperature of the rocks increases by depth. Depending on the lithology and stratigraphy the temperature of separate structures (Cretaceous, Maikop, Chokrak and others) change gradually.

Geothermic gradient and geothermal step were studied in each structure (Barda, Terter and Aghjabedy). As a result of the analysis it was defined that geothermic gradient decreases by depth, and geothermic step increases.

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