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Volume 46 Issue 2
Mar.  2024
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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2024  >  46(2): 319-332
WANG Daojun, CHEN Chao, LIU Zhujiang, YANG Shufan, LIU Miaomiao, XIE Jiatong. Main controlling factors for oil and gas enrichment in Jurassic laminated shale in Fuxing area of Sichuan Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2024, 46(2): 319-332. doi: 10.11781/sysydz202402319
Citation: WANG Daojun, CHEN Chao, LIU Zhujiang, YANG Shufan, LIU Miaomiao, XIE Jiatong. Main controlling factors for oil and gas enrichment in Jurassic laminated shale in Fuxing area of Sichuan Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2024, 46(2): 319-332. doi: 10.11781/sysydz202402319
shu

Main controlling factors for oil and gas enrichment in Jurassic laminated shale in Fuxing area of Sichuan Basin

doi: 10.11781/sysydz202402319

  • SINOPEC Exploration Company, Chengdu, Sichuan 610041, China

  • Received Date: 2023-12-08
  • Rev Recd Date: 2024-02-01
  • Publish Date: 2024-03-28
    Abstract
  • The Fuxing area of the Sichuan Basin is known for its multiple sets of organic-rich shale in the Jurassic period, with several wells yielding significant amounts of industrial oil and gas. Understanding the characteristics and factors influencing the enrichment of different shale facies sedimentary reservoirs is crucial for effective exploration. Through detailed rock core descriptions, experimental analysis, and drilling exploration, the author has classified and compared fine-grained sedimentary rock facies in terrestrial strata, characterized reservoirs, identified types of oil and gas reservoirs, and analyzed the main factors influencing enrichment and productivity. The study reveals that the Jurassic strata in the Fuxing area contain two sets of high-quality shale with semi-deep lacustrine facies: the first sub-section of the Dongyuemiao section of the Ziliujing Formation and the lower sub-section of the second section of the Lianggaoshan Formation. These shale layers exhibit multi-layer stacking, moderate TOC content, well-developed bedding, integrated source storage, and high gas/oil ratio characteristics. The lithology of these target shale layers is complex, leading to the establishment of a four-element lithofacies classification scheme based on "color-TOC-sedimentary structure-mineral composition". This scheme identifies the gray-black high carbon sand-laminated clay shale as the favorable lithofacies for the lower sub-section of the second section of the Lianggaoshan Formation, and the gray-black high carbon medium debris-laminated and fine sand medium debris-laminated clay shale as the favorable lithofacies for the eastern sub-section. The three lithofacies in the study area are horizontally distributed in a stable manner. The gray-black high carbon fine sand layer, medium debris layer, and fine sand-medium debris layer type clay shale exhibit reservoir characteristics of "porous coexistence, large pores and throats, and integrated pores and fractures". These reservoir properties, including good permeability, facilitate the efficient storage and flow of shale oil and gas in the pore-fracture storage system. The first sub-section of the Dongyuemiao section is a condensate gas reservoir, while the lower sub-section of the Lianggaoshan Formation's second section is a volatile oil reservoir. Key factors contributing to the enrichment of continental shale oil and gas have been identified, including medium to high hydrocarbon generation potential and strong retention rates supporting the accumulation of laminated shale oil and gas. A favorable hydrocarbon-diagenesis-reservoir formation configuration promotes oil and gas accumulation. Additionally, the development of micro cracks and suitable thermal evolution aids in hydrocarbon enrichment and flow, while large, wide, gentle synclines and high-pressure overpressure conditions support the sustained preservation of hydrocarbons.

     

    • All authors disclose no relevant conflict of interests.
    WANG Daojun proposed the overall concept of the paper. WANG Daojun, YANG Shufan and LIU Miaomiao were responsible for the research analysis and compilation of the paper. The manuscript was drafted and revised by WANG Daojun, CHEN Chao, LIU Zhujiang and XIE Jiatong. All the authors have read the last version of paper and consented for submission.
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