Resource potential of the Chernyshev Swell (the Timan Pechora Basin) in the context of the structure and petroleum habitat of the salt bearing thrust belts
https://doi.org/10.18599/grs.2022.1.4
Abstract
The salt bearing thrust belts are among the most prolific petroleum provinces in the world, including the fold belts flanking the Persian Gulf Basin, the Tarim Basin, the Terek-Sunzha Zone of the Eastern PreCaucasus etc. They are characterized by peculiar structural styles of deformation, large oil and gas pool sizes, significant flow rates. The Chernyshev Swell is among prospective salt bearing thrust belts. It is located in the Cis-Uralian part of the Timan Pechora Basin. Several exploration wells have been drilled in the area so far failed to deliver the anticipated oil and gas deposits. Post mortem study indicated that the main reason for the past failures was the mismatch between the complexities of the geological settings and the used exploration technologies. Integrated study of the area, conducted by the North Uralian Petroleum Company, using modern technologies, including 3D seismic surveying and magnetotelluric sounding, has enabled a far better understanding of this area’s structure and petroleum habitat. It is shown that high petroleum potential is attributed to the transition zone between the Chernyshev Swell and the Kosyu Rogov Foredeep Basin. This study indicated that the area of the Povarnitsa High is of priority interest for explration. This area provides supplementary opportunities in addition to the commercialization of the petroleum exploration potential. It includes production of rare earth and metals in brine of the evaporate deposits. The subsalt reservoirs of the Chernyshev Swell could be used for the storage of gas and CO2 sequestration. Integrated development of the resource potential of the Povarnitsa High may become a key driver of the economic development of the north-eastern part of the Republic of Komi.
About the Author
K. O. SobornovRussian Federation
Konstantin O. Sobornov – DSc (Geology and Mineralogy), Chief Geologist
Kievskoe sh. 1, Rumyantsevo Business park, build. 1, 412-а, Moscow, 142784
References
1. Antoshkina A.I. (2009). Genesis of the Upper Ordovician carbonate breccias of the Chernyshev Ridge. Vestnik Instituta geologii Komi NTs UrO RAN, 12, pp. 9–13. (In Russ.)
2. Bandaletova A.A., Gavrilov A.Yu., Galin E.V. (2021). Extraction of lithium from associated waters on the example of the Orenburg oil and gas condensate field. Proneft, 1(19), pp. 29–32. (In Russ.). https://ntc.gazpromneft.ru/research-and-development/proneft/4070/73172/
3. Bazhenova T.K., Bogoslovsky S.A. (2012). Results of computational modeling of oil and gas formation in the troughs of the Timan-Pechora basin. Report. Proc. Conf.: “Comprehensive study and development of the raw material base of oil and gas in the north of the European part of Russia”. St.Petersburg: VNIGRI. (In Russ.)
4. Biteau J., Blaizot M., Janodet D., de Clarens Ph. (2014). Recent emerging paradigms in hydrocarbon exploration. First Break, 32, pз. 49–58. https://doi.org/10.3997/1365-2397.2013035
5. Belenitskaya G.A. (2020). Salts of the Earth: tectonic, kinematic and magmatic aspects of geological history. Moscow: Geos, 605 p. (In Russ.)
6. Bushnev, D.A., Burdel’naya, N.S. & Zhuravlev, A.V. (2017). Organic matter in Upper Devonian deposits of the Chernyshev Ridge. Geochem. Int., 55, pp. 548–558. https://doi.org/10.1134/S0016702917060027
7. Callot J.P., Guichong W., Moretti I., Yongxing G., Letouzey J., Wu S. (2013). Structural style of a compressive wedge with salt and coal shale decollement levels. Analogue and seismic modeling of the Kuqa Thrust Belt (North Tarim, China). EGU General Assembly Conference Abstracts, p. 7860.
8. Danilov V.N. (2017). Chernyshev swell: geological structure and oil and gas potential. St.Petersburg: Renome, 288 p. (In Russ.)
9. Danshchikova I.I., Maydl T.V., Mityusheva T.P. (2019). Epigenetic changes in carbonate rocks and their relationship with the chemical composition of water in the Upper Ordovician-Lower Devonian oil and gas complex of the Chernyshev Ridge and the eastern side of the Khoreyver depression. Neftegazovaya geologiya. Teoriya i praktika, 14(3). (In Russ.). https://ngtp.ru/upload/iblock/ffa/44_2019.pdf
10. Duffy O.D., Dooly T.P., Hudec M.R., Jackson M.P.A., Fernandez N., Jackson C.A-L., Soto J.I. (2018). Structural evolution of salt-influenced foldand-thrust belts: A synthesis and new insight basins containing isolated salt diapirs. J. of Structural geology, 114, pp. 206–221. https://doi.org/10.1016/j.jsg.2018.06.024
11. Dusseault M.B., Bachu S, Rothenburg L. (2004). Sequestration of CO2 in salt caverns. Journal of Canadian Petroleum Technology, 43(11), pp. 49–55. https://doi.org/10.2118/04-11-04
12. Filimonova I.V., Nemov V.Yu., Provornaya I.V. et al. (2021). Oil and gas complex of Russia. Part 1. Oil industry 2020: long-term trends and state of the art. Novosibirsk: INGG SO RAN, 88 p. (In Russ.)
13. Grunis E.B., Rostovshchikov V.B., Bogdanov B.P. (2016). Ordovician Salts and Their Role in the Structure and Oil and Gas Potential of the Northeast of the Timan-pechora Province. Georesursy = Georesources, 18(1), pp. 13–23. https://doi.org/10.18599/grs.18.1.3
14. Jeroen M. Peters, Jacek B. Filbrandt, John P. Grotzinger, Mark J. Newall, Mark W. Shuster, Hisham A. Al-Siyabi (2003). Surface-piercing salt domes of interior North Oman, and their significance for the Ara carbonate ‘stringer’ hydrocarbon play. GeoArabia, 8(2), pp. 231–270. https://doi.org/10.2113/geoarabia0802231
15. Kendall J, Vergės J., Koshnaw R., Louterbach M. (2019). Petroleum tectonic comparison of fold and thrust belts: the Zagros of Iraq and Iran, the Pyrenees of Spain, the Sevier of Western USA and the Beni Sub-Andean of Bolivia. From: Hammerstein, J. A., Di Cuia, R., Cottam, M. A., Zamora, G. & Butler, R. W. H. (eds). Fold and Thrust Belts: Structural Style, Evolution and Exploration. Geological Society, London, Special Publications, 490. https://doi.org/10.1144/SP490-2018-102
16. Kotik I.S., Kotik O.S. (2018). Organic matter of the carbonaceous Middle Frasnian deposits of the Kosyu-Rogovskaya depression and the Chernyshev ridge (Timan-Pechora basin). Neftegazovaya geologiya. Teoriya i praktika, 13(3). (In Russ.). http://www.ngtp.ru/rub/1/24_2018.pdf
17. Li W., Chen Z., Huang P., Yu Z., Lu X. (2021). Formation of overpressure system and its relationship with the distribution of large gas fields in typical foreland basins in central and western China. Petroleum Exploration and Development, 48(3), pp. 625–640. https://doi.org/10.1016/S1876-3804(21)60050-2
18. Morton M.Q. (2015). River of Oil –Early Oil Exploration in Iraq. GeoExPro, 12(1). https://www.geoexpro.com/articles/2015/04/river-of-oil-early-oil-exploration-in-iraq
19. Neng Y., Tang Y., Yan D. (2021). Structural models in the ultra-deep layer of the Kuqa salt-bearing fold-and-thrust belt, West China. 82th EAGE Annual Conference and Exibition. Amsterdam, pp. 1–5. https://doi.org/10.3997/2214-4609.202112521
20. Nalivkin D.V. (1948). Feodosiy Nikolaevich Chernyshev. People of Russian science. Moscow-Leningrad, v. 1. (In Russ.)
21. Palshin N.A, Sobornov K.O., Bolourchi M.J., Aleksanova E.D., Yakovlev D.V., Aliyari A., Yakovlev A.G. (2021). Magnetotelluric studies of fold belts. Geofizika, 4, pp. 81–95. (In Russ.)
22. Sobornov K.O., Tarasov P.P. (1992). Allochthonous structure of the Kosyu-Rogovskaya depression (Polar Urals). Dokl. AN SSSR, 317(2), pp. 430–433. (In Russ.)
23. Sobornov K.O., Danilov V.N. (2015). The Chernyshev Swell: Supertrap or Waste Zone? Paper presented at the SPE Russian Petroleum Technology Conference, Moscow, Russia. doi: https://doi.org/10.2118/176614-MS
24. Sobornov K.O. (2019). Wedge-shaped thrusts of the southern flank of the Terek-Caspian foredeep: structure, development and petroleum prospectivity. Geologiya nefti i gaza, 6, pp. 19–30. (In Russ.). https://doi.org/10.31087/0016-7894-2019-6-19-30
25. Sobornov K.O., Korotkov I.P., Yakovlev D.V., Kulikov V.A., Kudryavtsev K.Yu., Kolesnik V.F. (2021). Squeezed diapirs of the Chernyshev Swell (the Timan Pechora Basin): integrated study and petroleum habitat. Geologiya nefti i gaza, 1, pp. 73–88. (In Russ.). DOI: 10.31087/0016-7894-2021-1-73-88
26. Sternbach, C.A. (2020). Super basin thinking: Methods to explore and revitalize the world’s greatest petroleum basins. AAPG Bulletin, 104(12), pp. 2463–2506. https://doi.org/10.1306/09152020073
27. Timonin N.I. (1975). Tectonics of the Chernyshev Swell. Leningrad: Nauka, 130 p. (In Russ.)
28. Yudin V.V. (1985). Layer-by-layer failures in the cover of the east of the Pechora plate are a possible object of hydrocarbon search. In: Pechora oil and gas basin, Tr. IG Komi FAN SSSR, v. 52. Syktyvkar, pp. 38–45. (In Russ.)
29. Zharkov V.A., Gubenok G.P., Chupriyanovskaya G.A. et al. (2015). State geological map of the Russian Federation. Scale 1:200,000. Second edition. Series Polar-Ural. Sheet Q-40-XVII, XVIII (Kosyuw). Explanatory letter. Moscow: VSEGEI, 274 p. (In Russ.)
Review
For citations:
Sobornov K.O. Resource potential of the Chernyshev Swell (the Timan Pechora Basin) in the context of the structure and petroleum habitat of the salt bearing thrust belts. Georesursy = Georesources. 2022;24(1):36-50. (In Russ.) https://doi.org/10.18599/grs.2022.1.4