留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

滇东曲靖地区下寒武统筇竹寺组泥页岩储层特征研究

白名岗 张聪 杨玉茹 代峰 熊杰

白名岗, 张聪, 杨玉茹, 等, 2017. 滇东曲靖地区下寒武统筇竹寺组泥页岩储层特征研究. 地质力学学报, 23 (6): 838-845.
引用本文: 白名岗, 张聪, 杨玉茹, 等, 2017. 滇东曲靖地区下寒武统筇竹寺组泥页岩储层特征研究. 地质力学学报, 23 (6): 838-845.
BAI Minggang, ZHANG Cong, YANG Yuru, et al., 2017. THE CHARACTERISTICS OF SHALE RESERVOIR FROM QIONGZHUSI FORMATION IN LOWER CAMBRIAN IN QUJING AREA, EASTERN YUNNAN PROVINCE, CHINA:A CASE STUDY OF WELL QUYE NO.1. Journal of Geomechanics, 23 (6): 838-845.
Citation: BAI Minggang, ZHANG Cong, YANG Yuru, et al., 2017. THE CHARACTERISTICS OF SHALE RESERVOIR FROM QIONGZHUSI FORMATION IN LOWER CAMBRIAN IN QUJING AREA, EASTERN YUNNAN PROVINCE, CHINA:A CASE STUDY OF WELL QUYE NO.1. Journal of Geomechanics, 23 (6): 838-845.

滇东曲靖地区下寒武统筇竹寺组泥页岩储层特征研究

基金项目: 

国家科技重大专项项目 2016ZX05034-003-006

地质矿产调查评价专项项目 DD2016178

详细信息
    作者简介:

    白名岗(1962-), 男, 大专, 工程师, 从事页岩气、天然气水合物等非常规油气基础地质调查和实验测试研究。E-mail:baimg1551@163.com

    通讯作者:

    张聪(1986-), 女, 博士研究生, 工程师, 主要从事页岩气基础地质调查和相关实验测试研究。E-mail:zh_cong520@qq.com

  • 中图分类号: P618.13

THE CHARACTERISTICS OF SHALE RESERVOIR FROM QIONGZHUSI FORMATION IN LOWER CAMBRIAN IN QUJING AREA, EASTERN YUNNAN PROVINCE, CHINA:A CASE STUDY OF WELL QUYE NO.1

  • 摘要: 下寒武统筇竹寺组页岩是南方页岩气勘查开发重点关注的层位之一,但滇东地区下寒武统筇竹寺组黑色页岩储层研究程度较低。样品采自2014年新钻的曲页1井,对下寒武统筇竹寺组黑色泥页岩进行全岩和粘土矿物X衍射分析、TOC、岩石物性、比表面积等测试和扫描电镜实验,综合分析了滇东曲靖地区筇竹寺组泥页岩储层特征及孔隙类型。结果表明:滇东曲靖地区下寒武统筇竹寺组泥页岩矿物组成主要是石英(44.75%)、粘土矿物(25.47%)、长石(16.44%);发育粒间孔、粒内孔和有机孔3种类型孔隙;有机质孔隙发育,以中孔为主,具有一定的页岩气勘探开发潜力;页岩储层自上而下孔隙体积有逐渐变小的趋势,但在井深400 m~500 m发育高孔隙体积;泥页岩储集性能的重要指标—孔隙度主要受有机质含量及发育程度的制约。

     

  • 图  1  工区地质简图及曲页1井位置

    F1—小江断裂;F2—鲁冲-车乌大断层;F3—宣威断层;F4—昭通-曲靖隐伏深大断裂;F5—十里铺断层;F6—法戛大断层;F7—弥勒-师宗深大断裂

    Figure  1.  Geological map of the study area and the location of Well Quye NO. 1

    图  2  曲页1井下寒武统筇竹寺组采样点及地层柱状图

    Figure  2.  Sampling sites and stratum histogram in lower Cambrian Qiongzhusi formation, Well Quye NO. 1

    图  3  曲页1井下寒武统筇竹寺组泥页岩矿物成分及粘土矿物含量

    Figure  3.  Mineral composition and clay content of shales in Qiongzhusi formation in lower Cambrian, Well Quye NO. 1

    图  4  曲页1井下寒武统筇竹寺组泥页岩矿物成分纵向变化特征

    Figure  4.  Vertical variation of mineral composition of shales in Qiongzhusi formation in lower Cambrian, Well Quye NO. 1

    图  5  曲页1井下寒武统筇竹寺组泥页岩储集空间类型

    a-粘土矿物粒间;b-溶蚀孔;c-溶蚀孔;d-有机质孔

    Figure  5.  Scanning electron microscope images of pore types in shales in Qiongzhusi formation in lower Cambrian, Well Quye NO.1

    图  6  曲页1井下寒武统筇竹寺组泥页岩中孔体积纵向变化特征

    Figure  6.  Vertical variation of mesopore volume of shales in Qiongzhusi formation in lower Cambrian, Well Quye NO.1

    图  7  曲页1井筇竹寺组黑色页岩中孔体积和有机碳、石英含量关系

    Figure  7.  Corelation between the mesopore volumn and the content of TOC & quartz in the dark shales in the Qiongzhusi formation, Well Quye NO. 1

    表  1  曲页1井下寒武统筇竹寺组泥页岩孔隙度和渗透率

    Table  1.   Porosity vs. permeability of shales in Qiongzhusi formation in lower Cambrian, Well Quye NO. 1

    样品
    编号
    埋深
    /m
    孔隙度
    /%
    渗透率
    /×10-3μm2
    QY1-Y57 276.03 1.78 0.0193
    QY1-Y56 281.26 1.56 0.0184
    QY1-J4 295.03 2.18 0.0136
    QY1-J5 301.94 3.01 0.0275
    QY1-Y52 302.95 1.94 0.0196
    QY1-Y50 313.75 1.35 0.0476
    QY1-Y48 324.29 1.73 0.0149
    QY1-J9 326.42 2.45 0.0361
    QY1-Y47 328.54 1.69 0.0190
    QY1-Y46 333.39 1.14 0.0188
    QY1-J13 362.48 2.57 0.0275
    QY1-Y41 371.07 1.64 0.0170
    QY1-Y40 378.8 2.24 0.0153
    QY1-J16 388.19 2.00 0.0116
    QY1-J18 402.37 1.18 0.0030
    QY1-J19 415.83 0.77 0.0076
    QY1-J21 430.6 1.82 0.0110
    QY1-J23 442.31 0.86 0.0103
    QY1-Y33 442.75 1.94 0.0429
    QY1-J25 451.23 1.18 0.0121
    QY1-J27 457.06 2.10 0.0088
    QY1-Y32 457.66 2.34 0.0399
    QY1-J29 463.02 1.59 0.0067
    QY1-J31 469.14 1.61 0.0117
    QY1-Y30 471.00 1.72 0.0308
    QY1-J32 474.12 1.72 0.0078
    QY1-Y28 484.47 2.17 0.0256
    QY1-J34 484.64 1.81 0.0077
    QY1-Y27 492.56 0.91 0.0211
    QY1-J36 496.78 1.43 0.0113
    QY1-Y26 498.44 0.38 0.0179
    QY1-Y25 501.06 0.48 0.0279
    QY1-J38 513.22 1.07 0.0103
    QY1-Y22 523.81 1.88 0.0255
    QY1-Y20 535.75 0.81 0.0276
    QY1-J40 535.91 1.89 0.0073
    QY1-Y18 547.95 0.26 0.0104
    QY1-Y17 552.47 1.47 0.0150
    QY1-Y16 556.93 0.37 0.0183
    QY1-Y14 567.17 1.65 0.0162
    QY1-Y13 572.19 1.15 0.0095
    下载: 导出CSV

    表  2  曲页1井下寒武统筇竹寺组泥页岩比表面积测试结果

    Table  2.   Test results of specific surface area of shales in Qiongzhusi formation in lower Cambrian, Well Quye NO. 1

    样品编号 QY1-J1 QY1-J5 QY1-J9 QY1-J11 QY1-J13 QY1-J15 QY1-J19 QY1-J21 QY1-J23 QY1-J25 QY1-J27 QY1-J32 QY1-J36 QY1-J38 QY1-J40
    井深/m 245.75 301.94 326.42 338.15 362.48 382.89 415.83 430.6 442.31 451.23 457.06 474.12 496.78 513.22 535.91
    表面积/(m2/g) 5.3130 3.9960 4.0330 3.2980 2.0870 2.8000 10.5310 6.1420 1.8000 4.3920 4.2500 4.7990 8.2760 1.9500 2.6860
    孔隙体积/(ml/g) 0.0103 0.0076 0.0074 0.0068 0.0050 0.0060 0.0147 0.0116 0.0030 0.0072 0.0096 0.0081 0.0118 0.0042 0.0054
    平均孔径/nm 3.8690 3.7985 3.6923 4.1234 4.8119 4.2959 2.7823 3.7632 3.3439 3.2928 4.5177 3.3714 2.8579 4.2600 4.0343
    下载: 导出CSV
  • [1] 李新民. 我国首个超千亿立方米页岩气田诞生[OL]. http://www.mlr.gov.cn/xwdt/mtsy/xinhuanet/201407/t20140722_1324552.htm.

    LI Xinmin. The birth of China's first billion cubic meters of shale gas field[OL]. http://www.mlr.gov.cn/xwdt/jrxw/201407/t20140722_1324457.htm.2014, 7.22. (in Chinese)
    [2] 郭旭升.南方海相页岩气"二元富集"规律-四川盆地及周缘龙马溪组页岩气勘探实践认识[J].地质学报, 2014, 88(7):1209~1218. https://mall.cnki.net/qikan-DZXE201407001.html

    GUO Xusheng. Rules of two~factor enrichiment for marine shale gas in Sourthern China-Understanding from the Longmaxi formation shale gas in Sichuan basin and its surroungding area[J]. Geological Journal, 2014, 88(7):1209~1218. (in Chinese with English abstract) https://mall.cnki.net/qikan-DZXE201407001.html
    [3] 郭彤楼, 张汉荣.四川盆地焦石坝页岩气田形成与富集高产模式[J].石油勘探与开发, 2014, 41(1):28~36. doi: 10.11698/PED.2014.01.03

    GUO Tonglou, ZHANG Hanrong. Formation and enrichment mode of Jiaoshiba shale gas field, Sichuan basin[J]. Petroleum Exploration and Development, 2014, 41(1):28~36. (in Chinese with English abstract) doi: 10.11698/PED.2014.01.03
    [4] 王玉芳, 翟刚毅, 王劲铸, 等.四川盆地及周缘龙马溪组页岩产气效果影响因素[J].地质力学学报, 2017, 23(4):540~547. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20170405&flag=1

    WANG Yufang, ZHAI Gangyi, WANG Jinzhu, et al. Factors influencing gas production effectiveness of Longmaxi formation shale in Sichun basin and adjacent areas[J]. Journal of Geomechanics, 2017, 23(4):540~547. (in Chinese with English abstract) http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20170405&flag=1
    [5] 程克明, 王世谦, 董大忠, 等.上扬子区下寒武统筇竹寺组页岩气成藏条件[J]..天然气工业, 2009, 29(5):40~44. http://www.oalib.com/paper/4982341

    CHENG Keming, WANG Shiqian, DONG Dazhong, et al. Accumulation conditions of shale gas reservoirs in the lower Cambrian Qiongzhusi formation, the upper Yangtze region[J]. Natural Gas Industry, 2009, 29(5):40~44. (in Chinese with English abstract) http://www.oalib.com/paper/4982341
    [6] 张聪, 包书景, 石砥石, 等.云南曲靖地区下寒武统筇竹寺组页岩气成藏地质条件及有利区预测[J].海相油气地质, 2017, 22(1):69~74. http://www.oalib.com/paper/4982341

    ZHANG Cong, BAO Shujing, SHI Dishi, et al. Geological conditions for shale gas accumulation and favorable area prediction in Qujing of Eastern Yunnan[J]. Marine Origin Petroleum Geology, 2017, 22(1):69~74. (in Chinese with English abstract) http://www.oalib.com/paper/4982341
    [7] 王丽波, 久凯, 曾维特, 等.上扬子黔北地区下寒武统海相黑色泥页岩特征及页岩气远景区评价[J].岩石学报, 2013, 29(9):3263~3278. http://d.wanfangdata.com.cn/Periodical/ysxb98201309024

    WANG Libo, JIU kai, ZENG Weiye, et al. Characteristics of lower Cambrian marine black shales and evaluation of shale gas prospective area in Qianbei area, upper Yangtze region[J]. Acta Petrologica Sinica, 2013, 29(9):3263~3278. (in Chinese with English abstract) http://d.wanfangdata.com.cn/Periodical/ysxb98201309024
    [8] 周新桂, 刘和甫, 王宗秀, 等.我国叠合盆地油气调查战略思考[J].地质力学学报, 2011, 17(2):111~120. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20110201&flag=1

    ZHOU Xingui, LIU Hepu, WANG Zongxiu, et al. Thoughts of strategic Hydrocabron survey on superimposed basins in China[J]. Journal of Geomechanics, 2011, 17(2):111~120. (in Chinese with English abstract) http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20110201&flag=1
    [9] 杨勤生.滇东下古生界页岩气成藏层位及远景[J].云南地质, 2010, 29(1):1~6. http://www.cqvip.com/qk/95791X/201001/33201747.html

    YANG Qinsheng. The horizon & potentiality of lower Palaeozoic shale gas deposit in East Yunnan[J]. Yunnan Geology, 2010, 29(1):1~6. (in Chinese with English abstract) http://www.cqvip.com/qk/95791X/201001/33201747.html
    [10] 梁兴, 叶熙, 张介辉, 等.滇黔北下古生界海相页岩气藏赋存条件评价[J].海相油气地质, 2011, 16(4):11~21. http://www.cnki.com.cn/Article/CJFDTotal-HXYQ201104004.htm

    LIANG Xing, YE Xi, ZHANG Jiehui, et al. Evaluation of preservation conditions of lower Paleozoic marine shale gas reservoirs in the Northern part of Dianqianbei depression[J]. Marine Origin Petroleum Geology, 2011, 16(4):11~21.(in Chinese with English abstract) http://www.cnki.com.cn/Article/CJFDTotal-HXYQ201104004.htm
    [11] 梁兴, 叶熙, 张介辉, 等.滇黔北坳陷威信凹陷页岩气成藏条件分析与有利区优选[J].石油勘探与开发, 2011, 38(6):641~6519. http://www.wenkuxiazai.com/doc/c2c0399ddd88d0d233d46a31-2.html

    LIANG Xing, YE Xi, ZHANG Jiehui, et al. Reservoir forming conditions and favorable exploration zones of shale gas in the Weixin sag, Dianqianbei depression[J]. Petroleum Exploration and Development, 2011, 38(6):693~699. (in Chinese with English abstract) http://www.wenkuxiazai.com/doc/c2c0399ddd88d0d233d46a31-2.html
    [12] 云南省地质矿产局.云南省岩石地层[M].北京:中国地质大学出版社, 1996. 21~45.

    Bureau of Geology and Mineral Resources of Yunnan Province. Rock Strata in Yunnan Province[M]. Beijing:China University of Geosciences Press, 1996, 21~45. (in Chinese)
    [13] 云南省地质矿产局.云南省区域地质志[M].北京:地质出版社, 1990. 1~728.

    Bureau of Geology and Mineral Resources of Yunnan Province. Regional Geology of Yunnan Province[M]. Beijing:Geological Publishing House, 1990. 1~728. (in Chinese)
    [14] 云南省地质矿产局.云南省岩相古地理图集[M].昆明:云南科技出版社, 1995. 53~60.

    Bureau of Geology and Mineral Resources of Yunnan Province. Atlas of the Palaeo Geography of Yunnan Province[M]. Kunming:Yunnan Science and Technology Press, 1995. 53~60. (in Chinese)
    [15] Rouquerol J, Avnir D, Fairbridge C W, et al. Recommendations for the characterization of porous solids[J]. Pure Applied Chemistry, 1994, 66(8):1739~1758. http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.460.3717
    [16] Ross D J K, Bustin R M. The importance of shale composition and pore structure upon gas storage potential of shale gas reservoirs[J]. Marine and Petroleum Geology, 2009, 26(6):916~927. doi: 10.1016/j.marpetgeo.2008.06.004
    [17] 蒲泊伶, 董大忠, 耳闯, 等.川南地区龙马溪组页岩有利储层发育特征及其影响因素[J].天然气工业, 2013, 33(12):41~47. http://www.doc88.com/p-4562199214457.html

    PU Boling, DONG Dazhong, ER Chuang, et al. Favorable reservoir characteristics of the Longmaxi shale in the southern Sichuan basin and their influencing factors[J]. Natural Gas Industry, 2013, 33(12):41~47. (in Chinese with English abstract) http://www.doc88.com/p-4562199214457.html
    [18] 杨峰, 宁正福, 胡昌蓬, 等.页岩储层微观孔隙结构特征[J].石油学报, 2013, 34(2):301~311. doi: 10.7623/syxb201302012

    YANG Feng, NING Zhengfu, HU Changpeng, et al. Characterization of microscopic pore structures in shale reservoirs[J]. Acta Petrolei Sinica, 2013, 34(2):301~311. (in Chinese with English abstract) doi: 10.7623/syxb201302012
    [19] 于炳松.页岩气储层的特殊性及其评价思路和内容[J].地学前缘, 2012, 19(3):252~258. http://d.wanfangdata.com.cn/Periodical/dxqy201203027

    YU Bingsong. Particularity of shale gas reservoir and its evaluation[J]. Earth Science Frontiers, 2012, 19(3):252~258. (in Chinese with English abstract) http://d.wanfangdata.com.cn/Periodical/dxqy201203027
    [20] 于炳松.页岩气储层孔隙分类与表征[J].地学前缘, 2013, 20(4):211~220. https://mall.cnki.net/qikan-CXYY201715138.html

    YU Bingsong. Classification and characterization of gas shale pore system[J]. Earth Science Frontiers, 2013, 20(4):211~220. (in Chinese with English abstract) https://mall.cnki.net/qikan-CXYY201715138.html
  • 加载中
图(7) / 表(2)
计量
  • 文章访问数:  322
  • HTML全文浏览量:  279
  • PDF下载量:  25
  • 被引次数: 0
出版历程
  • 收稿日期:  2017-01-18
  • 刊出日期:  2017-12-01

目录

    /

    返回文章
    返回