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基于埋深变化的川南龙马溪组页岩孔隙特征及控制因素分析

陈洋, 唐洪明, 廖纪佳, 罗超, 赵圣贤, 郑马嘉, 钟权. 2022. 基于埋深变化的川南龙马溪组页岩孔隙特征及控制因素分析[J]. 中国地质, 49(2): 472-484. doi: 10.12029/gc20220209
引用本文: 陈洋, 唐洪明, 廖纪佳, 罗超, 赵圣贤, 郑马嘉, 钟权. 2022. 基于埋深变化的川南龙马溪组页岩孔隙特征及控制因素分析[J]. 中国地质, 49(2): 472-484. doi: 10.12029/gc20220209
CHEN Yang, TANG Hongming, LIAO Jijia, LUO Chao, ZHAO Shengxian, ZHENG Majia, ZHONG Quan. 2022. Analysis of shale pore characteristics and controlling factors based on variation of buried depth in the Longmaxi Formation, Southern Sichuan Basin[J]. Geology in China, 49(2): 472-484. doi: 10.12029/gc20220209
Citation: CHEN Yang, TANG Hongming, LIAO Jijia, LUO Chao, ZHAO Shengxian, ZHENG Majia, ZHONG Quan. 2022. Analysis of shale pore characteristics and controlling factors based on variation of buried depth in the Longmaxi Formation, Southern Sichuan Basin[J]. Geology in China, 49(2): 472-484. doi: 10.12029/gc20220209

基于埋深变化的川南龙马溪组页岩孔隙特征及控制因素分析

  • 基金项目:
    国家自然科学青年基金项目(41702164)及中石油-西南石油大学创新联合体项目“川南深层海相页岩气地质-工程双甜点预测理论与关键技术研究”(2020CX020102)资助
详细信息
    作者简介: 陈洋,男,1995年生,硕士生,矿产普查与勘探专业; E-mail: 1693206037@qq.com
    通讯作者: 唐洪明,男,1966年生,教授,博士生导师,主要从事油气藏地质学和储层保护技术的研究与教学工作; E-mail: swpithm@vip.163.com
  • 中图分类号: P618.13

Analysis of shale pore characteristics and controlling factors based on variation of buried depth in the Longmaxi Formation, Southern Sichuan Basin

  • Fund Project: Supported by National Natural Science Youth Fund Project (No.41702164) and CNPC-Southwest Petroleum University Innovation Consortium Project 'Research on prediction theory and key technology of deep-seated marine shale gas geology-engineering dual sweet spots in southern Sichuan' (No.2020CX020102)
More Information
    Author Bio: CHEN Yang, male, born in 1995, master candidate, major in mineral survey and exploration; E-mail: 1693206037@qq.com .
    Corresponding author: TANG Hongming, male, born in 1966, professor, doctoral supervisor, mainly engaged in the research and teaching of oil and gas reservoir geology and reservoir protection technology; E-mail: swpithm@vip.163.com
  • 研究目的

    中国浅层-中深层页岩气勘探开发技术已经趋于成熟,深层页岩成为下一步勘探开发的重点,探明不同埋深条件下页岩的孔隙特征及其控制因素利于推动深层页岩的评优选区工作。

    研究方法

    本文基于核磁共振、场发射扫描电镜和X-射线衍射等实验分析手段,对比性评价了川南地区不同深度的龙马溪组页岩孔隙度、孔隙结构参数特征并进行影响因素分析。

    研究结果

    随着埋深的增加,总孔隙度呈现下降的趋势; 3000 m以浅、3000~3500 m和3500 m以深页岩孔隙度主体分别为4%~8%、3%~7%和3%~6%。不同埋深龙马溪组页岩孔隙类型与大小分布无显著差异,各深度段页岩均发育大量纳米级有机质孔隙、矿物粒间孔、粒内溶孔和微裂缝。

    结论

    高U/Th比和低Ti含量下形成的丰富有机质是深层页岩孔隙发育的关键因素; 高硅质矿物含量和高地层压力系数对页岩储层孔隙起到了保护作用,减缓了上覆地层的压实作用,但埋深过大仍会导致页岩孔隙减少、孔隙度降低。

  • 加载中
  • 图 1  川南地区沉积特征与井位分布图(修改自马新华等,2018)

    Figure 1. 

    图 2  典型井龙马溪组页岩TOC和孔隙度对比图

    Figure 2. 

    图 3  典型井龙马溪组页岩孔隙度分布频率

    Figure 3. 

    图 4  川南龙马溪组富有机质页岩孔隙度与埋深关系图

    Figure 4. 

    图 5  龙马溪组富有机质页岩孔隙度分布图

    Figure 5. 

    图 6  不同埋深龙马溪组页岩孔径分布

    Figure 6. 

    图 7  深埋条件下龙马溪组页岩孔隙扫描电镜照片

    Figure 7. 

    图 8  不同深度龙马溪组页岩TOC与与孔隙度关系图

    Figure 8. 

    图 9  不同小层页岩TOC和孔隙度的关联性及TOC与沉积环境关系

    Figure 9. 

    图 10  3500 m以深页岩矿物含量与孔隙度相关性(a,b)及不同岩相页岩孔隙度分布频率图(c)

    Figure 10. 

    图 11  压力系数与埋深关系(a)、不同深度段孔隙度与压力系数相关性(b, c, d)

    Figure 11. 

    表 1  不同埋深下压力系数与孔隙度统计表

    Table 1.  Statistical table of pressure coefficient and porosity at different depths

    下载: 导出CSV
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出版历程
收稿日期:  2020-10-21
修回日期:  2021-01-05
刊出日期:  2022-04-25

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