东尼日尔盆地群上白垩统Donga组沉积体系及勘探潜力

袁圣强; 姜虹; 汤戈; 肖坤叶; 刘邦; 潘春浮; 王海荣; 毛凤军; 郭郁; 周川闽

doi:10.3799/dqkx.2022.464

Volume 48 Issue 2

Feb. 2023

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Article Navigation > Earth Science > 2023 > 48(2): 705-718

Yuan Shengqiang, Jiang Hong, Tang Ge, Xiao Kunye, Liu Bang, Pan Chunfu, Wang Hairong, Mao Fengjun, Guo Yu, Zhou Chuanmin, 2023. The Sedimentary System and Hydrocarbon Potential of Upper Cretaceous Donga Formation, East Niger Basin Group. Earth Science, 48(2): 705-718. doi: 10.3799/dqkx.2022.464

Citation:

Yuan Shengqiang, Jiang Hong, Tang Ge, Xiao Kunye, Liu Bang, Pan Chunfu, Wang Hairong, Mao Fengjun, Guo Yu, Zhou Chuanmin, 2023. The Sedimentary System and Hydrocarbon Potential of Upper Cretaceous Donga Formation, East Niger Basin Group. Earth Science, 48(2): 705-718. doi: 10.3799/dqkx.2022.464

Citation:

Yuan Shengqiang, Jiang Hong, Tang Ge, Xiao Kunye, Liu Bang, Pan Chunfu, Wang Hairong, Mao Fengjun, Guo Yu, Zhou Chuanmin, 2023. The Sedimentary System and Hydrocarbon Potential of Upper Cretaceous Donga Formation, East Niger Basin Group. Earth Science, 48(2): 705-718. doi: 10.3799/dqkx.2022.464

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The Sedimentary System and Hydrocarbon Potential of Upper Cretaceous Donga Formation, East Niger Basin Group

doi: 10.3799/dqkx.2022.464

1.
Research Institute of Petroleum Exploration & Development, PetroChina, Beijing 100083, China
2.
Research Institute of Petroleum Exploration and Development of Dagang Oilfield, PetroChina, Tianjin 300280, China
3.
China National Oil and Gas Exploration and Development Corporation, Beijing 100034, China
4.
School of Energy Resources, China University of Geosciences, Beijing 100083, China

Received Date: 2022-11-21
Publish Date: 2023-02-25

Abstract

Abstract

The East Niger basin group belongs to the West African Rift System. Based on seismic, drilling, side wall core, and geochemical analysis data of Donga formation, this paper analyses its depositional system, play and exploration potential. Donga formation is a normal cycle sequence formed in late Cretaceous transgression, and the top is developed with thin carbonate rocks. This sequence is widely developed in the Upper Cretaceous of the East Niger Basin Group, which indicates that seawater flooded these basins during the Late Cretaceous and forms a temporarily unified basin. The transgression event significantly affected the sedimentary system of the Late Cretaceous basin and controlled its petroleum system and hydrocarbon accumulation. The widely deposited mudstone can be a good hydrocarbon source rock and cap rock. There are two plays in Donga formation, upper generation and lower reservoir, supply hydrocarbon laterally, and self⁃generated and self⁃stored. Reservoir is the control factor of Donga formation hydrocarbon accumulation, the moderate buried and near provenance area in the north and southeast margin could develop good reservoir and has good exploration potential.
- Eastern Niger,
- Termit basin,
- Upper Cretaceous,
- sedimentary system,
- hydrocarbon potential,
- Donga Formation,
- petroleum geology

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References(39)

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The Sedimentary System and Hydrocarbon Potential of Upper Cretaceous Donga Formation, East Niger Basin Group

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