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陆相和海相页岩储层孔隙结构差异性分析
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  • 英文篇名:Analysis of differences in pore structure between continental and marine shale reservoirs
  • 作者:李廷微 ; 姜振学 ; 宋国奇 ; 李政 ; 朱日房 ; 苏思远 ; 陈委涛 ; 宁传祥 ; 王智 ; 薛子鑫
  • 英文作者:LI Tingwei;JIANG Zhenxue;SONG Guoqi;LI Zheng;ZHU Rifang;SU Siyuan;CHEN Weitao;NING Chuanxiang;WANG Zhi;XUE Zixin;State Key Laboratory of Petroleum Resources and Prospecting,China University of Petroleum(Beijing);Natural Gas Hydrate Engineering Technology Center,Guangzhou Marine Geological Survey;Shengli Oilfield Company,SINOPEC;Exploration and Development Research Institute,Shengli Oilfield Company,SINOPEC;Patent Examination Cooperation Sichuan Center of the Patent Office,CNIPA;
  • 关键词:陆相 ; 海相 ; 页岩储层 ; 孔隙结构 ; 差异性
  • 英文关键词:lacustrine facies;;marine facies;;shale reservoirs;;pore structure;;difference
  • 中文刊名:YQCS
  • 英文刊名:Petroleum Geology and Recovery Efficiency
  • 机构:中国石油大学(北京)油气资源与探测国家重点实验室;广州海洋地质调查局天然气水合物工程技术中心;中国石化胜利油田分公司;中国石化胜利油田分公司勘探开发研究院;国家知识产权局专利局专利审查协作四川中心;
  • 出版日期:2019-01-03 13:31
  • 出版单位:油气地质与采收率
  • 年:2019
  • 期:v.26;No.136
  • 基金:国家“973”计划“页岩油富集成藏的边界地质条件及动力学特征”(2014CB239105)
  • 语种:中文;
  • 页:YQCS201901007
  • 页数:7
  • CN:01
  • ISSN:37-1359/TE
  • 分类号:69-75
摘要
页岩储层以微-纳米孔隙和裂缝作为页岩油气的赋存空间,对其孔隙结构特征的研究是明确页岩油气富集机理的关键,而陆相和海相页岩储层的孔隙结构特征存在巨大的差异。为此,运用场发射扫描电镜、CO_2吸附、N_2吸附、高压压汞分析和索氏抽提等方法,以沾化凹陷沙三段下亚段陆相页岩储层和川东南龙马溪组海相页岩储层为典型实例,深入分析陆相和海相页岩储层的孔隙结构差异。结果表明,沾化凹陷沙三段下亚段陆相页岩储层中有机质单体内部并未发育密集分布且相互连通的蜂窝状孔隙,具有极大孔体积的宏孔更为发育,能够为游离烃赋存提供良好的储集空间,控制着页岩油的富集。而川东南龙马溪组海相页岩储层中有机质单体内部密集发育相互连通的蜂窝状孔隙,具有极大比表面积的微孔最为发育,能够为吸附烃赋存提供足够的比表面,控制着页岩气的富集。
        Since shale oil and gas occur in micro-to nano-pores and fractures,researches on pore structure characteristics of shale reservoirs are important to understand the accumulation mechanism of shale oil and gas. There are great differences in pore structure between continental and marine shale reservoirs. In order to analyze their differences in pore structure,several methods including field emission-scanning electron microscopy,CO_2 adsorption,N_2 adsorption,high-pressure mercury injection,and Soxhlet Extraction,etc. were applied to analyze samples from the lower submember of 3rd member of Eocene Shahejie Formation(Es_3~l)continental shale in Zhanhua Sag and Longmaxi Formation marine shale in Sichuan Basin.The results show that interconnected honeycomb-shape pores are not developed within organic matter for Es_3~l shale in Zhanhua Sag. In addition,macro-pores with great pore volume are well-developed,providing good spaces for free hydrocarbon storage and controlling shale oil accumulation. In contrast,interconnected honeycomb-shape pores are well-developed within organic matter for Longmaxi Formation marine shale in Sichuan Basin. Micropores with great specific surface area provide sufficient spaces for absorbed hydrocarbon and control shale gas accumulation.
引文
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