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The scientific interest of evaluating the thermal regime of various areas has come to the fore with a more complete understanding that all major processes inside the Earth are related to thermal events and that all physical properties of rocks, as a basis for observed geophysical phenomena, are more or less dependent on temperature. The characterization of the thermal regime is followed by the basic elements: temperature and geothermal gradient, thermal conductivity and geothermal flow. The quantitative study of g...