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SUN Zhongliang，ZHANG Kuihua，SONG Zhenxiang，et al. Quality difference analysis of source rocks in Fengcheng Formation, Hashan area, Junggar Basin[J]. Bulletin of Geological Science and Technology，2026，45（1）：1-16 doi: 10.19509/j.cnki.dzkq.tb20240153
Citation: SUN Zhongliang，ZHANG Kuihua，SONG Zhenxiang，et al. Quality difference analysis of source rocks in Fengcheng Formation, Hashan area, Junggar Basin[J]. Bulletin of Geological Science and Technology，2026，45（1）：1-16 doi: 10.19509/j.cnki.dzkq.tb20240153
shu

Quality difference analysis of source rocks in Fengcheng Formation, Hashan area, Junggar Basin

doi: 10.19509/j.cnki.dzkq.tb20240153
  • 1 .

    Wuxi Research Institute of Petroleum Geology, RIPEP, SINOPEC, Wuxi, Jiangsu 214151, China

  • 2 .

    Exploration and Development Research Institute, Shengli Oilfield Company, SINOPEC, Dongying 257015, China

  • 3 .

    State Key Laboratory of Shale Oil and Gas Enrichment Mechanisms and Effective Development, Wuxi, Jiangsu 214151, China

  • 4 .

    Shengli Oilfield Company, SINOPEC, Dongying 257000, China

  • 5 .

    SINOPEC Key Laboratory of Petroleum Accumulation Mechanisms, Wuxi, Jiangsu 214151, China

More Information
  • Corresponding author: E-mail：sunzhl8188.sykg@sinopec.com
  • Received Date: 09 Apr 2024
  • Accepted Date: 16 Jul 2024
  • Rev Recd Date: 09 Jul 2024
    • Available Online: 26 Nov 2025
    Abstract
  • <p>The exploration of shale oil in the Permian Fengcheng Formation Hashan area shows <bold>promising momentum</bold>, with breakthroughs achieved in multiple shale oil exploration wells. Early research indicates that the Fengcheng Formation in the Hashan area is mainly composed of four lithofacies: terrigenous clastic lithofacies, dolomitic mixed lithofacies, volcanic clastic-bearing mixed lithofacies, and alkaline mineral-bearing mixed lithofacies, with <bold>the development of various types of source rocks</bold>. </p></sec><sec><title>Objective

    To further evaluate the quality of source rocks in the Fengcheng Formation of the Hashan area and the factors influencing their quality,

    Methods

    this study starts with the sedimentary background, conducts a detailed evaluation of the source rocks in the Fengcheng Formation by lithofacies, identifies lithofacies with high-quality source rocks, and on this basis, analyzes the factors affecting source rock quality to clarify the directions for exploration.

    Results

    The results show that among the mudstones in the Fengcheng Formation of the Hashan area, the volcanic clastic-bearing mixed lithofacies exhibits the highest organic matter abundance, while the dolomitic mixed lithofacies has the greatest hydrocarbon generation potential. The kerogen of the mudstones in the Fengcheng Formation of the Hashan area is mainly Type I–II. The maturity of mudstones in the western section of Hashan ranges from 0.8% to 0.97%, and in the middle section, it is mainly between 1.2% and 1.37%.

    Conclusion

    The quality of source rocks in the Fengcheng Formation of the Hashan area is mainly controlled by sedimentary environment, hydrocarbon-generating parent material, maturity, alkaline minerals, and volcanic activity. Organic matter in dolomitic mixed lithofacies and alkaline mineral-bearing mixed lithofacies is more enriched in deep-water, reducing, medium-to-high salinity, and arid environments. In contrast, organic matter in terrigenous clastic lithofacies and volcanic clastic-bearing mixed lithofacies is more enriched in relatively shallow-water, oxygen-poor, low-salinity, and arid–semi-arid environments. Green algae (Dunaliella-like) that developed in high-salinity areas of the sedimentary center exhibit higher oil and gas conversion rates, enabling the mudstones of dolomitic mixed lithofacies to have high hydrocarbon generation potential even with low organic matter abundance. An increase in maturity and alkaline minerals reduces the measured values of TOC (Total Organic Carbon) and hydrocarbon generation potential, while an appropriate amount of volcanic clastics provides favorable conditions for the enrichment of organic matter.

     

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