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Heat flow and presence of oil and gas (the Yamal peninsula, Tomsk region)

V.I. Isaev, G.A. Lobova, A.N. Fomin, V.I. Bulatov, S.G. Kuzmenkov, M.F. Galieva, D.S. Krutenko

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DOI https://doi.org/10.18599/grs.2019.3.125-135

125-135
rus.
eng.

open access

Under a Creative Commons license

The possibilities of Geothermy as a geophysical method are studied to solve forecast and prospecting problems of Petroleum Geology of the Arctic regions and the Paleozoic of Western Siberia. Deep heat flow of Yamal fields, whose oil and gas potential is associated with the Jurassic-Cretaceous formations, and the fields of Tomsk Region, whose geological section contents deposits in the Paleozoic, is studied. The method of paleotemperature modeling was used to calculate the heat flow density from the base of a sedimentary section (by solving the inverse problem of Geothermy). The schematization and mapping of the heat flow were performed, taking into account experimental determinations of the parameter. Besides, the correlation of heat flow features with the localization of deposits was revealed. The conceptual and factual basis of research includes the tectonosedimentary history of sedimentary cover, the Mesozoic-Cenozoic climatic temperature course and the history of cryogenic processes, as well as lithologic and stratigraphic description of the section, results of well testing, thermometry and vitrinite reflectivity data of 20 deep wells of Yamal and 37 wells of Ostanino group of fields of Tomsk region. It was stated that 80 % of known Yamal deposits correlate with anomalous features of the heat flow. Bovanenkovskoe and Arkticheskoe fields are located in positive anomaly zones. 75 % of fields of Ostanino group relate to anomalous features of the heat flow. It is shown that the fields, which are characterized by existence of commercial deposits in the Paleozoic, are associated with the bright gradient zone of the heat flow. The forecast of commercial inflows in the Paleozoic for Pindzhinskoe, Mirnoe and Rybalnoe fields is given. The correlation between the intensity of naftidogenesis and the lateral inhomogeneity of the deep heat flow is characterized as a probable fundamental pattern for Western Siberia.

 

the deep heat flow, oil and gas fields, Yamal, Paleozoic, Tomsk Region, the correlation, Western Siberia

 

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Valery I. Isaev
National Research Tomsk Polytechnic University; Ugra State University
30, Lenin ave., Tomsk, 634050, Russian Federation
Phone: +7 (3822) 701-777 ad. 2942, e-mail: isaevvi@tpu.ru

Galina A. Lobova
National Research Tomsk Polytechnic University
30, Lenin ave., Tomsk, 634050, Russian Federation

Alexander N. Fomin
Trofimuk Institute of Petroleum Geology and Geophysics of Siberian Branch of Russian Academy of Sciences
3, Ak. Koptyug ave., Novosibirsk, 630090, Russian Federation

Valery I. Bulatov
Yugra State University
16, Chekhov st., Khanty-Mansiysk, 628012, Russian Federation

Stanislav G. Kuzmenkov
Ugra State University
16, Chekhov st., Khanty-Mansiysk, 628012, Russian Federation

Margarita F. Galieva
National Research Tomsk Polytechnic University
30, Lenin ave., Tomsk, 634050, Russian Federation

Daniil S. Krutenko
National Research Tomsk Polytechnic University
30, Lenin ave., Tomsk, 634050, Russian Federation

 

For citation:

Isaev V.I., Lobova G.A., Fomin A.N., Bulatov V.I., Kuzmenkov S.G., Galieva M.F., Krutenko D.S (2019). Heat flow and presence of oil and gas (the Yamal peninsula, Tomsk region). Georesursy = Georesources, 21(3), pp. 125-135. DOI: https://doi.org/10.18599/grs.2019.3.125-135