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Geochemical characteristics of the Yogou Formation of the Termit Basin (Niger)

https://doi.org/10.32454/0016-7762-2025-67-4-39-48

Abstract

Background. Hydrocarbon deposits in Niger have been actively explored since the 1970s. However, oil production only commenced in 2011 with the discovery of the Agadem oil field. The available hydrocarbon resources of this region are currently underestimated; thus, it is relevant to forecast the territory for oil and gas content using modern integrated geological and geophysical methods and studies. To that end, the available hydrocarbon systems in the region, including source rock formations, reservoir rocks, sealing rock, reservoir traps should be determined. Additionally, the way these elements are related to each other should be studied. This article examines the source rock formations of the Termit Basin in the Republic of Niger. The region is of considerable interest due to the oil and gas prospects of the Yogou Formation.

Aim. To examine the geochemical characteristics of the Yogou Formation through identifying the organic matter source of the Yogou Formation mudstones, as well as specifying the predominant phase composition of hydrocarbons generated by mudstones of the Yogou Formation.

Materials and methods. Samples of the Yogou Formation mudstones from nine wells located in the Agadem Block of the Termit Basin were used. The results of pyrolytic, petrographic, and biomarker studies of the Yogou Formation source rock kerogen obtained from stock materials, published pa- pers, and reports provided by the Ministry of Petroleum Resources of the Republic of Niger, were analyzed.

Results. Petrographic analysis performed by the China National Petroleum Corporation revealed that the kerogen of the source rocks of the Yogou Formation has a maceral composition including vitrinite, inertinite, and liptinite, particularly leptodetrinite, sporinite, cutinite, and resistinite. Analysis of the biomarker content of the extracted samples of the Yogou Formation showed that C27-C28-C29 steranes are present in the extracts with a predominance of C29 steranes over the common C27 and C28 steranes. According to the initial hydrogen index values determined by Rock-Eval pyrolysis, the predominant source for organic matter was higher vegetation.

Conclusion. The organic matter of the rocks of the Yogou Formation was originally derived from higher terrestrial vegetation. Consequently, the source rocks will generate more gaseous hydro-arbons.

About the Authors

M. A. Abdel’ Kader
National University of Oil and Gas “Gubkin University”
Russian Federation

Mahaman Abass Abdel’ Kader — graduate student

65, bld. 1, Leninsky Ave., Moscow 119991

tel.: +7 (925) 850-91-18


Competing Interests:

the authors declare no conflict of interest



V. V. Chernova
National University of Oil and Gas “Gubkin University”
Russian Federation

Viktoriya V. Chernova — laboratory assistant

65, bld. 1, Leninsky Ave., Moscow 119991

tel.: +7 (499) 507-84-32

+7 (903) 315-47-38


Competing Interests:

the authors declare no conflict of interest



L. V. Miloserdova
National University of Oil and Gas “Gubkin University”
Russian Federation

Lyudmila V. Miloserdova — Cand. Sci. (Geol.-Mineral.), docent

65, bld. 1, Leninsky Ave., Moscow 119991


Competing Interests:

the authors declare no conflict of interest



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For citations:


Abdel’ Kader M.A., Chernova V.V., Miloserdova L.V. Geochemical characteristics of the Yogou Formation of the Termit Basin (Niger). Proceedings of higher educational establishments. Geology and Exploration. 2025;67(4):39-48. (In Russ.) https://doi.org/10.32454/0016-7762-2025-67-4-39-48

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