China Petroleum Exploration ›› 2025, Vol. 30 ›› Issue (1): 156-167.DOI: 10.3969/j.issn.1672-7703.2025.01.012

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New progress in the study of hydrocarbon accumulation and exploration insights in Central and Western African Rift System

Shi Zhongsheng1,Ma Feng1,Pang Wenzhu2,Chen Bintao1,Xue Juo1,Dai Hansong1,Xu Fei1,Ma Lun1   

  1. 1 PetroChina Research Institute of Petroleum Exploration and Development-Northwest; 2 China National Oil and Gas Exploration and Development Co., Ltd.
  • Online:2025-01-15 Published:2025-01-15

Abstract: There are multiple petroliferous basins in Central and Western African Rift System (CWARS), with abundant oil and gas resources.Based on the study of the control of CWARS basins orientation and regional stress field direction on basin formation, relationship between tectonic evolution of CWARS and source rock development, as well as the sedimentary filling and hydrocarbon accumulation patterns of rift basins in different directions, the author presents the latest study progress of basin formation, hydrocarbon generation and hydrocarbon accumulation in CWARS. In addition, hydrocarbon accumulation patterns in various types of basins and exploration practice in typical basins are analyzed, which clarify the high-efficiency exploration practices and future exploration fields and orientations in CWARS. The study results show that, controlled by basin orientation and direction of regional stress field, multi-stage superimposed and single-stage rift basins were developed in CWARS. Among them, multi-stage rift processes occurred in NW–SE trending basins in the Early Cretaceous, Late Cretaceous,and Paleogene, forming the main hydrocarbon accumulation pattern of “lower source rock and upper reservoir, and hydrocarbon accumulation above source rock”. While a single-stage rift process experienced in the NE–SW trending basins in the Early Cretaceous, forming hydrocarbon accumulation patterns of “integrated source rock and reservoir, and hydrocarbon accumulation inside source rock” in the Lower Cretaceous and “upper source rock and lower reservoir, and hydrocarbon accumulation below source rock” in the Lower Cretaceous and buried hill.The diverse tectonic settings and geological evolution processes determined that terrigenous marine source rock was developed in the Upper Cretaceous in Western African Rift System and continental facies source rock was developed in the Lower Cretaceous in Central African Rift System. The thick, high-quality and mature source rocks provided a material basis for hydrocarbon enrichment in CWARS. The exploration practice in Melut Basin indicates that the key to achieving the high-efficiency exploration of overseas oil and gas projects relies on the rapid identification of oil-rich sags and the subsequent deployment of connected 3D seismic data. The major fields and orientations for the future exploration in CWARS include intra-source rock hydrocarbon accumulation combination in NW-SE trending multi-stage superimposed rift basins such as Termit and Melut, intra-source rock lithological oil reservoirs in NE-SW trending single-stage rift basins such as Bongor and Doseo, as well as traps outside source rock in oil-rich sags.

Key words: hydrocarbon accumulation pattern, oil-rich sag, high-efficiency exploration, outside source rock play, Central and Western African Rift System

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