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    吴仕玖, 曾德铭, 王兴志, 李顺, 陈虎, 王岩. 川中龙岗—营山地区雷口坡组雷四3亚段储层成岩作用及孔隙演化[J]. 中国地质, 2013, 40(3): 919-826.
    引用本文: 吴仕玖, 曾德铭, 王兴志, 李顺, 陈虎, 王岩. 川中龙岗—营山地区雷口坡组雷四3亚段储层成岩作用及孔隙演化[J]. 中国地质, 2013, 40(3): 919-826.
    WU Shi-jiu, ZENG De-ming, WANG Xin-zhi, LI Shun, CHEN Hu, WANG Yan. Reservoir diagenesis and porosity evolution of Leikoupo-43 Formation in Longgang-Yingshan area of central Sichuan Basin[J]. GEOLOGY IN CHINA, 2013, 40(3): 919-826.
    Citation: WU Shi-jiu, ZENG De-ming, WANG Xin-zhi, LI Shun, CHEN Hu, WANG Yan. Reservoir diagenesis and porosity evolution of Leikoupo-43 Formation in Longgang-Yingshan area of central Sichuan Basin[J]. GEOLOGY IN CHINA, 2013, 40(3): 919-826.

    川中龙岗—营山地区雷口坡组雷四3亚段储层成岩作用及孔隙演化

    Reservoir diagenesis and porosity evolution of Leikoupo-43 Formation in Longgang-Yingshan area of central Sichuan Basin

    • 摘要: 提要:四川盆地中部龙岗—营山地区中三叠统雷口坡组雷四3亚段储层发育较好,在颗粒型白云岩中显示丰富的油气,具有良好的勘探前景。通过对研究区30余口钻井岩心、薄片的宏观及微观观察,结合地球化学特征,对成岩作用类型及特征进行较详细的研究,探讨了成岩作用与储集空间演化的关系。研究发现区内雷四3亚段储层成岩演化过程复杂,各种成岩作用发育,储层质量的好坏受成岩作用影响明显。压实压溶作用、多期胶结作用以及多期充填作用导致粒间孔、晶间孔大幅度减少;混合水白云石化作用、表生期和埋藏期溶蚀作用以及构造破裂作用是优质储层形成的关键,形成了大量的粒间溶孔、粒内溶孔、晶间溶孔和溶蚀缝,成为现今该层段的主要储集空间。

       

      Abstract: Abstract:Good reservoirs are developed in the Middle Triassic Leikoupo-43 Formation in Longgang-Yingshan area of central Sichuan basin. There exist rich oil and gas resources in granular dolomite, suggesting good exploration prospect. Through macro- and micro- observation of thin sections and rocks from more than ten wells in combination with geochemical characteristics, the authors made a detailed investigation into diagenetic types and characteristics and examined the relationship between the diagenesis and the evolution of reservoir space. The findings show that the diagenetic evolution process of reservoir in the Middle Triassic Leikoupo-43 Formation in Longgang-Yingshan area of central Sichuan basin was complex, and during this process various diagenetic actions were developed, with the reservoir quality being clearly affected by the diagenesis.The compaction and pressure solution, multiphase cementation and multiphase packing action resulted in substantial reduction of intergranular pores and intercrystalline pores. The mixed water dolomitization, the supergene and burial dissolution and the tectonic disruption constituted the keys to the formation of high quality reservoir and the generation of massive intergranular dissolution pores,intragranular dissolution pores, intercrystalline dissolved pores and eroded fissures, which have now became the main oil and gas reservoir space.

       

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