Analysis of geothermal parameters at the oil and gas fields in Dnieper-Donets basin
The current work performs the comparison of distribution of geothermal gradient depending on the display of hydrogeological inversion and location of hydrocarbon deposits. On the example of Yarmolintsivske and Machuske fields is shown that the increase of the gradient takes place at the intersection of the roof of the deposit. The average geothermal gradient over deposit is set to 19-20 °C/km in both cases.