China Petroleum Exploration ›› 2024, Vol. 29 ›› Issue (5): 44-60.DOI: 10.3969/j.issn.1672-7703.2024.05.005

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Geological characteristics and exploration prospects of the Mesoproterozoic Changcheng System in Ordos Basin

Liu Gang1,2,Yang Wenjing2,3,Jing Xianghui1,2,Bai Haifeng1,2,Shi Baohong4,Sun Yaping5,Ren Junfeng1,2,Pan Xing1,2,Zhang Jianwu1,2,Wei Jiayi1,2   

  1. 1 Research Institute of Exploration & Development, PetroChina Changqing Oilfield Company; 2 National Engineering Laboratory for Exploration and Development of Low Permeability Oil & Gas Fields; 3 Exploration Department, PetroChina Changqing Oilfield Company; 4 Xi’an Shiyou University; 5 Changqing Supervision Company, CNPC Chuanqing Drilling Engineering Co., Ltd.
  • Online:2024-09-14 Published:2024-09-14

Abstract: The Mesoproterozoic Changcheng System was the first set of sedimentary cap rocks in Ordos Basin, with a wide distribution area but low degree of study and exploration. By using field outcrops, drilling results of risk exploration well PT1, and 3D seismic data, a systematic study is conducted on stratigraphic correlation and distribution, sedimentary facies, and source rock characteristics in the Changcheng System. In Ordos Basin, five sets of formations were developed in Changcheng System from bottom to top, including Xiong’er Group, Baicaoping Formation, Beidajian Formation, Cuizhuang Formation, and Luoyukou Formation. The stratigraphic distribution characteristics vary in various rift troughs. In Jinshan rift trough, the five sets of formations were developed completely. In Dingbian rift trough, three sets of formations were developed, including Xiong’er Group, Baicaoping Formation and Beidajian Formation. While only Beidajian Formation was developed in Helan rift trough. The bathyal–shallow marine–coastal–delta sedimentary system was dominant in Changcheng System, intercalated with tidal flat deposits. Effective source rock in Cuizhuang Formation was encountered in Zhongtiaoshan in Xiong’er rift and several exploration wells in the secondary rift troughs, with the highest organic carbon content of 1.52% and average Ro of 2.32%, showing potential of large-scale hydrocarbon generation. The basin thermal evolution simulation shows that Cuizhuang Formation source rock entered the mature stage in the Middle Permian with Ro value of 0.5%, and entered dry gas generation stage in the late stage of the Early Cretaceous with Ro of 2.0%. The comprehensive study shows that the configuration between source rock and reservoir in Changcheng System was good in Ordos Basin, forming self-generation and self-storage type natural gas reservoirs. Furthermore, two exploration targets are optimally selected in Dingbian rift trough and Jinshan rift trough, providing direction for gas exploration “towards source rock” in deep formations in the basin.

Key words: Ordos Basin, Mesoproterozoic, Changcheng System, Cuizhuang Formation, sedimentary facies, source rock, exploration prospect

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