The Geochemical Characteristics of Fluid Inclusions as Indicators of the Degree of Organic Matter Transformation in Jurassic Sediments of the Em-Egovskaya Summit (Krasnoleninsky Arch, Western Siberia)

Fluid inclusions in quartz crystals from the Abalak formation carbonate rocks of five wells on the Em-Egovskaya summit of the Krasnoleninsky arch (Western Siberia) were investigated. Two-phase fluid inclusions with water-salt solutions, inclusions containing organic liquid, and single-phase gas fluid inclusions were found. For fluid inclusions with two-phases, the homogenization temperatures were obtained. For single-phase inclusions, the temperature of the second phase forming was revealed. It was established that two types of primary inclusions are present in one well, that is, with oil and with a water–salt solution. The homogenization temperature of the primary fluid inclusion containing a water–salt solution is 267°C, the homogenization of the oil-containing inclusion exceeds 300°C. In primary–secondary inclusions, the homogenization temperature reached 136°C. Studies of the composition of inclusions by infrared spectrometry have shown that in single-phase inclusions, the gas is represented by methane. In primary–secondary inclusions, the composition may vary, while in the gas phase, the predominant components may be hydrocarbons with two or more carbon atoms. Studies of organic matter from the deposits of the Tutleim source-rock formation overlying the Abalak formation have shown that the stage of catagenetic transformation of kerogen in the studied wells changes. It was found that in wells in which organic matter is most transformed, the homogenization temperature of fluid inclusions exceeds 130°C. Thus, it has been proved that on the territory of the Em-Egovskaya summit of the Krasnoleninsky arch, Jurassic deposits were affected by heat flows created by high-temperature fluids. Not only were rocks of the Abalak formation exposed by thermal processes, but also organic matter from the Tutleim formation was changed; as a result its maturity increased and the generation of hydrocarbon compounds was stimulated. The results we obtained explain the difference in the catagenetic transformation of the organic matter of the Tutleim formation in this area. The study of the molecular composition of inclusions will allow us to more accurately reconstruct the conditions of hydrothermal processes. The study of fluid inclusions makes it possible to develop new criteria for the search for oil and gas deposits.