| 应用氩离子抛光-扫描电镜方法研究四川九老洞组页岩微观孔隙特征 |
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| 引用本文： | 王羽,金婵,汪丽华,王建强,姜政,王彦飞,普洁.应用氩离子抛光-扫描电镜方法研究四川九老洞组页岩微观孔隙特征[J].岩矿测试,2015,34(3):278-285. |
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| 作者姓名： | 王羽 金婵 汪丽华 王建强 姜政 王彦飞 普洁 |
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| 作者单位： | 中国科学院微观界面物理与探测重点实验室, 上海 201800;中国科学院上海应用物理研究所上海光源, 上海 201204,中国科学院微观界面物理与探测重点实验室, 上海 201800;中国科学院上海应用物理研究所上海光源, 上海 201204,中国科学院微观界面物理与探测重点实验室, 上海 201800;中国科学院上海应用物理研究所上海光源, 上海 201204,中国科学院微观界面物理与探测重点实验室, 上海 201800;中国科学院上海应用物理研究所上海光源, 上海 201204,中国科学院微观界面物理与探测重点实验室, 上海 201800;中国科学院上海应用物理研究所上海光源, 上海 201204,中国科学院地质与地球物理研究所, 北京 100029,中国科学院微观界面物理与探测重点实验室, 上海 201800;中国科学院上海应用物理研究所上海光源, 上海 201204 |
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| 基金项目： | 中国科学院战略性先导科技专项(B类)——页岩三维成像实验技术和数据获取技术(XDB10020102);上海市科学技术委员会基础研究重点项目、页岩微观结构的同步辐射研究(12JC1410400) |
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| 摘 要： | 微观孔隙结构是页岩储层研究的重点,而扫描电镜方法无法识别机械抛光中由于页岩硬度差异所造成的不规则形貌。本文利用氩离子抛光-扫描电镜方法对四川威远区块九老洞组页岩进行研究,发现了三种孔隙类型:1无机孔以粒间孔和黏土矿物层间孔为主,同时发育晶间孔和生物孔,孔径主体100~500 nm;2有机孔受控于热成熟度或有机黏土复合体,孔径范围数十纳米至数微米;3微裂缝包括成岩收缩裂缝、高压碎裂缝、构造裂缝和人为裂缝,缝宽数微米,缝长数微米至数十微米。研究表明无机孔和微裂缝是九老洞组页岩气的主要储集空间。
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| 关 键 词： | 微观孔隙结构 氩离子抛光 扫描电子显微镜 四川盆地 九老洞组页岩 |
| 收稿时间： | 2015/4/11 0:00:00 |
| 修稿时间： | 5/6/2015 12:00:00 AM |
Characterization of Pore Structures of Jiulaodong Formation Shale in the Sichuan Basin by SEM with Ar-ion Milling |
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| WANG Yu,JIN Chan,WANG Li-hu,WANG Jian-qiang,JIANG Zheng,WANG Yan-fei and PU Jie.Characterization of Pore Structures of Jiulaodong Formation Shale in the Sichuan Basin by SEM with Ar-ion Milling[J].Rock and Mineral Analysis,2015,34(3):278-285. |
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| Authors: | WANG Yu JIN Chan WANG Li-hu WANG Jian-qiang JIANG Zheng WANG Yan-fei and PU Jie |
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| Institution: | Key Laboratory of Interfacial Physics and Technology, Shanghai Institute of Applied Physics, Chinese Academy of Sciences, Shanghai 201800, China;Shanghai Synchrotron Radiation Facility, Shanghai Institute of Applied Physics, Chinese Academy of Sciences, Shanghai 201204, China,Key Laboratory of Interfacial Physics and Technology, Shanghai Institute of Applied Physics, Chinese Academy of Sciences, Shanghai 201800, China;Shanghai Synchrotron Radiation Facility, Shanghai Institute of Applied Physics, Chinese Academy of Sciences, Shanghai 201204, China,Key Laboratory of Interfacial Physics and Technology, Shanghai Institute of Applied Physics, Chinese Academy of Sciences, Shanghai 201800, China;Shanghai Synchrotron Radiation Facility, Shanghai Institute of Applied Physics, Chinese Academy of Sciences, Shanghai 201204, China,Key Laboratory of Interfacial Physics and Technology, Shanghai Institute of Applied Physics, Chinese Academy of Sciences, Shanghai 201800, China;Shanghai Synchrotron Radiation Facility, Shanghai Institute of Applied Physics, Chinese Academy of Sciences, Shanghai 201204, China,Key Laboratory of Interfacial Physics and Technology, Shanghai Institute of Applied Physics, Chinese Academy of Sciences, Shanghai 201800, China;Shanghai Synchrotron Radiation Facility, Shanghai Institute of Applied Physics, Chinese Academy of Sciences, Shanghai 201204, China,Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China and Key Laboratory of Interfacial Physics and Technology, Shanghai Institute of Applied Physics, Chinese Academy of Sciences, Shanghai 201800, China;Shanghai Synchrotron Radiation Facility, Shanghai Institute of Applied Physics, Chinese Academy of Sciences, Shanghai 201204, China |
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| Abstract: | Microscopic pore structure is the key to studying shale gas reservoirs. Traditional Scanning Electron Microscope cannot be used to identify topographic irregularities caused by differential hardness of components during mechanical polishing. Microscopic pore structures of Jiulaodong formation shale in the Weiyuan area of the Sichuan basin were investigated using scanning electron microscope coupled with an Ar-ion milling technique. Three types of pores were identified: (1)mineral matrix pores (pore diameters are mostly 100-500 nm), mainly including interparticle pores and intraplatelet pores within clay aggregates, and intercrystalline pores within pyrite/anatase and biological pores; (2)organic matter pores (pore diameters range from tens of nanometers to several micrometers), either controlled by thermal evolution of kerogen or clay minerals coated by organic matter; (3)micro fractures (with length of dozens of micrometers and width of a few micrometers), including shrinkage fracture, tectonic fracture, overpressure fracture and artificial fracture. In conclusion, micro-nano pores in Jiulaodong shale are mainly composed of mineral matrix pores and micro fractures which provide the main storage space and flow channel for shale gas. |
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| Keywords: | microscopic pore structure Ar-ion milling Scanning Electron Microscope Sichuan Basin Jiulaodong Formation Shale |
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