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高校地质学报 ›› 2026, Vol. 32 ›› Issue (04): 534-546.DOI: 10.16108/j.issn1006-7493.2025039

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川东北大安寨段泥页岩孔隙发育特征及控制因素分析

彭 君1,杨雨秋2*,贾云倩2,黄 蕾3,周勇水3,雷 鸣2,姚素平2   

  1. 1. 中国石化 中原油田普光分公司,达州 636100;
    2. 南京大学 地球科学与工程学院,南京 210023;
    3. 中国石化 中原油田分公司勘探开发研究院,濮阳 457001
  • 出版日期:2026-08-20 发布日期:2026-08-20

Analysis of Pore Development Characteristics and Controlling Factors in Shale of the Da’anzhai Member, Northeastern Sichuan

PENG Jun1,YANG Yuqiu2*,JIA Yunqian2,HUANG Lei3,ZHOU Yongshui3,LEI Ming2,YAO Suping2   

  1. 1. Sinopec Zhongyuan Oilfield Puguang Branch, Dazhou 636100, China;
    2. School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, China;
    3. Exploration and Development Research Institute of Sinopec Zhongyuan Oilfield Company, Puyang 457001, China
  • Online:2026-08-20 Published:2026-08-20

摘要: 勘探实践表明,川东北地区侏罗系大安寨段页岩油气具有广阔的勘探前景,但其储层孔隙发育特征及控制因素缺乏深入研究。文章通过源储协同演化热模拟实验,探讨了大安寨段泥页岩成岩—成烃—成储协同演化过程。研究表明:有机质降解生烃、碱性矿物溶蚀、粘土矿物转化、石英矿物溶蚀是大安寨段泥页岩演化过程中主要的增孔因素,而碱性矿物重结晶、有机质芳构化、石英矿物次生加大是主要的减孔因素;根据有机质生烃演化曲线和矿物在热演化过程中的变化特征,半定量分析了热演化过程中有机质生烃和矿物转化对泥页岩孔隙发育的贡献,并建立了大安寨段泥页岩成岩—成烃—成储协同演化模式,将大安寨段泥页岩孔隙演化过程划分为四个阶段:中成岩A1期(Ro=0.79%~1.09%)、中成岩A2期(Ro=1.09%~1.28%)、中成岩B1期(Ro=1.28%~1.47%)和中成岩B2期(Ro=1.47%~2.02%),其中泥页岩孔隙增量主要发生在中成岩A2期,该阶段对应有机质大量生油阶段,表明大安寨段有机质生烃对泥页岩孔隙发育具有重要贡献,为进一步认识川东北大安寨储层演化规律提供重要参考。

关键词: 页岩孔隙演化, 源储协同演化模拟实验, 成岩作用, 成烃作用, 大安寨段, 川东北

Abstract: Exploration practice indicates that the Jurassic Da’anzhai Member shale oil and gas in northeastern Sichuan show
broad exploration prospects, yet in-depth research on shale pore development and its controlling factors remains lacking. This study investigates the co-evolutionary process of hydrocarbon generation, diagenesis, and reservoir formation in the Da’anzhai shale through source-reservoir coupled pyrolysis experiments. The research demonstrates that: organic matter degradation and hydrocarbon generation, alkaline mineral dissolution, clay mineral transformation, and quartz mineral dissolution constitute the primary pore-enhancing factors during the evolution of the Da’anzhai shale, while alkaline mineral recrystallization, organic matter aromatization, and quartz secondary enlargement represent the main pore-reducing factors. Based on the organichydrocarbon generation evolution curve and mineral alteration characteristics during thermal evolution, a semi-quantitative analysis was conducted on the contributions of organic hydrocarbon generation and mineral transformation to shale pore development throughout the thermal evolution process. Furthermore, a co-evolution model for diagenesis-hydrocarbon generationreservoir formation of the Da’anzhai Member shale was established, dividing the pore evolution processes of the Da’anzhai shale into four stages: The Middle Diagenetic substages A1 (Ro=0.79%-1.09%), A2 (Ro=1.09%-1.28%), B1 (Ro=1.28%-1.47%), and B2 (Ro=1.47%-2.02%) exhibit distinct evolutionary characteristics. Significant shale porosity increment primarily occurs during the Middle Diagenetic Substage A2, which corresponds to the peak oil generation stage of organic matter. This demonstrates that hydrocarbon generation from organic matter substantially contributes to pore development in the Da’anzhai Member shale, providing critical insights into understanding the reservoir evolution patterns in northeastern Sichuan’s Da’anzhai Formation.

Key words: shale pore evolution, source-reservoir coupled evolution simulation experiment, diagenesis, hydrocarbon generation;
Da’anzhai Member,
Northeastern Sichuan

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