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The paper is meant to prove that structural reconstruction of riftogenic basins is accompanied by the intensification of tectonichydrothermal activity. It controls the mobility of gaseous-liquid hydrocarbons during their primary and lateral migration in the process of deposit formation. The intensity index of tectonic-hydrothermal activation is equal to the ratio of maximum paleotemperatures of gaseous-liquid inclusions to the paleotemperatures calculated from vitrinite reflectance values. This parameter determined in the same intervals of a geologic section reflects the level of paleothermal incongruity in the natural system. It can be used to make predictive estimates of the areas for hydrocarbon materials. The values of this parameter vary in the range of 1.5–2.5 in promising riftogenic areas with the source rocks in the temperature zone of 80–160°С due to conducive heating.

Oil as the result of lithogenesis complicated by intensification of tectonic-hydrothermal activity (on the example of Western Siberia)