Abstract
This work presents the results of the electromagnetic study of thermal water deposits, conducted in the territory of the Bishkek geodynamic test area (Northern Tien Shan). The heat flow in this territory is quite high, which testifies in favor of the development of geothermal energy in the region. The objects with high electrical conductivity isolated in the geological environment by various electrical prospecting methods are fractured basement rocks saturated with a heated fluid (in a different aggregate state) in the upper part of the Earth’s crust, promising for the development of geothermal energy.
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