Geothermal Regime and Petroleum Potential of The Anadyr and Okhotsk–Kamchatka Basins

The study was designed to establish temperature dependence of the sedimentary cover and gas and oil fields at the Anadyr and Okhotsk-Kamchatka basins. A paleothermal and modern thermal field are determined by regional, zonal and local components. The first component depends on conductive flux, second and third are closely connected to convective heat transfer and influence of the oil and gas fields. The correlation between the hydrocarbon pools and the anomaly thermal field of the sedimentary basins by convective heat transfer are established