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    焦石坝地区五峰组-龙马溪组页岩纹层发育特征及其储集意义

    王超 张柏桥 舒志国 陆亚秋 包汉勇 杨文新 刘超 李凯

    王超, 张柏桥, 舒志国, 陆亚秋, 包汉勇, 杨文新, 刘超, 李凯, 2019. 焦石坝地区五峰组-龙马溪组页岩纹层发育特征及其储集意义. 地球科学, 44(3): 972-982. doi: 10.3799/dqkx.2019.018
    引用本文: 王超, 张柏桥, 舒志国, 陆亚秋, 包汉勇, 杨文新, 刘超, 李凯, 2019. 焦石坝地区五峰组-龙马溪组页岩纹层发育特征及其储集意义. 地球科学, 44(3): 972-982. doi: 10.3799/dqkx.2019.018
    Wang Chao, Zhang Boqiao, Shu Zhiguo, Lu Yaqiu, Bao Hanyong, Yang Wenxin, Liu Chao, Li Kai, 2019. Shale Lamination and Its Influence on Shale Reservoir Quality of Wufeng Formation-Longmaxi Formation in Jiaoshiba Area. Earth Science, 44(3): 972-982. doi: 10.3799/dqkx.2019.018
    Citation: Wang Chao, Zhang Boqiao, Shu Zhiguo, Lu Yaqiu, Bao Hanyong, Yang Wenxin, Liu Chao, Li Kai, 2019. Shale Lamination and Its Influence on Shale Reservoir Quality of Wufeng Formation-Longmaxi Formation in Jiaoshiba Area. Earth Science, 44(3): 972-982. doi: 10.3799/dqkx.2019.018

    焦石坝地区五峰组-龙马溪组页岩纹层发育特征及其储集意义

    doi: 10.3799/dqkx.2019.018
    基金项目: 

    中国博士后科学基金面上项目 2017M622559

    国家自然科学基金项目 41702149

    国家重大科技专项 2016ZX05060

    详细信息
      作者简介:

      王超(1987-), 男, 副研究员, 博士, 主要从事非常规油气资源评价及储层地球物理精细表征研究

    • 中图分类号: P618.13

    Shale Lamination and Its Influence on Shale Reservoir Quality of Wufeng Formation-Longmaxi Formation in Jiaoshiba Area

    • 摘要: 目前针对海相富有机质页岩纹层对储层品质的影响方面尚未开展深入研究.通过钻井岩心、薄片鉴定、氩离子抛光扫描电镜、核磁孔隙结构和扫描电镜矿物定量评价(QEMSCAN)等测试分析,将川东焦石坝地区五峰组-龙马溪组一段页岩纹层按矿物组分划分为硅质纹层、钙质纹层和粘土质纹层3类,并识别出水平纹层、杂积纹层、粒序纹层、侵蚀交错纹层和楔状交错纹层5类页岩纹层沉积构造.结合纹层发育密度和最大纹层厚度,划分出3个纹层发育段,每一段又细分为弱发育段和强发育段.综合纹层发育特征和页岩储层物性参数可知:纹层强发育段其总有机碳含量和有机质孔隙均相对减少,而无机质孔隙相对发育,纹层发育影响了页岩孔隙类型和孔径占比的分布.

       

    • 图  1  涪陵地区区域地质背景(a)、取心井位置(b)和JY-A井五峰组-龙马溪组综合柱状图(c)

      Fig.  1.  Regional geological background of Fuling area(a), core wells(b) and the integrated histogram of Wufeng Formation-Longmaxi Formation of Well JY-A (c)

      图  2  焦石坝地区龙马溪组页岩薄片及QEMSCAN矿物定量表征

      Fig.  2.  Photograph of thin sections and QEMSCAN of Longmaxi shale in Jiaoshiba area

      图  3  焦石坝地区五峰组-龙马溪组页岩纹层典型沉积构造

      a.水平纹层; b.杂积纹层; c.粒序纹层; d.侵蚀交错纹层; e.楔状交错纹层

      Fig.  3.  Typical sedimentary structure of laminae in Wufeng-Longmaxi shales in Jiaoshiba area

      图  4  焦石坝五峰组-龙马溪组页岩纹层发育特征综合柱状图

      Fig.  4.  The integrated histogram of laminae development of Wufeng-Longmaxi shales in Jiaoshiba area

      图  5  焦石坝五峰组-龙马溪组页岩不同开发小层纹层发育特征

      Fig.  5.  Laminae development characteristics of different Wufeng-Longmaxi shale layers in Jiaoshiba area

      图  6  总有机碳与孔隙度(a)和纹层密度(b)的关系

      Fig.  6.  Plots of TOC vs. porosity (a) and TOC vs. density (b)

      图  7  不同纹层发育段页岩微-纳米级孔隙镜下特征

      Fig.  7.  Pore characteristics of different laminae development section

      图  8  纹层发育段孔径分布同TOC相关性综合分析图

      Fig.  8.  Correlation analysis between pore size vs.TOC of laminae development section

    • [1] Bahk, J.J., Chough, S.K., Han, S.J., 2000.Origins and Paleoceanographic Significance of Laminated Muds from the Ulleung Basin, East Sea(Sea of Japan).Marine Geology, 162(2-4):459-477. https://doi.org/10.1016/s0025-3227(99)00079-1
      [2] Bour, I., Mattioli, E., Pittet, B., 2007.Nannofacies Analysis as a Tool to Reconstruct Paleoenvironmental Changes during the Early Toarcian Anoxic Event.Palaeogeography, Palaeoclimatology, Palaeoecology, 249(1-2):58-79. https://doi.org/10.1016/j.palaeo.2007.01.013
      [3] Caplan, M.L., Marc Bustin, R., 2001.Palaeoenvironmental and Palaeoceanographic Controls on Black, Laminated Mudrock Deposition:Example from Devonian-Carboniferous Strata, Alberta, Canada.Sedimentary Geology, 145(1-2):45-72. https://doi.org/10.1016/s0037-0738(01)00116-6
      [4] Chen, L., Lu, Y.C., Jiang, S., et al., 2015.Heterogeneity of the Lower Silurian Longmaxi Marine Shale in the Southeast Sichuan Basin of China.Marine and Petroleum Geology, 65:232-246. https://doi.org/10.1016/j.marpetgeo.2015.04.003
      [5] Chen, S.B., Han, Y.F., Fu, C.Q., et al., 2016.Micro and Nano-Size Pores of Clay Minerals in Shale Reservoirs:Implication for the Accumulation of Shale Gas.Sedimentary Geology, 342:180-190. https://doi.org/10.1016/j.sedgeo.2016.06.022
      [6] Cheng, M., Luo, X.R., Lei, Y.H., et al., 2015.The Distribution, Fractal Characteristic and Thickness Estimation of Silty Laminae and Beds in the Zhangjiatan Shale, Ordos Basin.Natural Gas Geoscience, 26(5):845-854 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/trqdqkx201505007
      [7] Curtis, M.E., Sondergeld, C.H., Ambrose, R.J., et al., 2012.Microstructural Investigation of Gas Shales in Two and Three Dimensions Using Nanometer-Scale Resolution Imaging.AAPG Bulletin, 96(4):665-677. https://doi.org/10.1306/08151110188
      [8] Dean, J.M., Kemp, A.E.S., Pearce, R.B., 2001.Palaeo-Flux Records from Electron Microscope Studies of Holocene Laminated Sediments, Saanich Inlet, British Columbia.Marine Geology, 174(1-4):139-158. https://doi.org/10.1016/s0025-3227(00)00147-x
      [9] Fauchille, A.L., Ma, L., Rutter, E., et al., 2017.An Enhanced Understanding of the Basinal Bowland Shale in Lancashire(UK), through Microtextural and Mineralogical Observations.Marine and Petroleum Geology, 86:1374-1390. https://doi.org/10.1016/j.marpetgeo.2017.07.030
      [10] Guo, T.L., 2016.Key Geological Issues and Main Controls on Accumulation and Enrichment of Chinese Shale Gas.Petroleum Exploration and Development, 43(3):317-326 (in Chinese with English abstract).
      [11] He, Z.L., Nie, H.K., Zhang, Y.Y., 2016.The Main Factors of Shale Gas Enrichment of Ordovician Wufeng Formation-Silurian Longmaxi Formation in the Sichuan Basin and Its Adjacent Areas.Earth Science Frontiers, 23(2):8-17 (in Chinese with English abstract).
      [12] Ilgen, A.G., Heath, J.E., Akkutlu, I.Y., et al., 2017.Shales at All Scales:Exploring Coupled Processes in Mudrocks.Earth-Science Reviews, 166:132-152. https://doi.org/10.1016/j.earscirev.2016.12.013
      [13] Kuroda, J., Ohkouchi, N., Ishii, T., et al., 2005.Lamina-Scale Analysis of Sedimentary Components in Cretaceous Black Shales by Chemical Compositional Mapping:Implications for Paleoenvironmental Changes during the Oceanic Anoxic Events.Geochimica et Cosmochimica Acta, 69(6):1479-1494. https://doi.org/10.1016/j.gca.2004.06.039
      [14] Leclair, S.F., Arnott, R.W.C., 2005.Parallel Lamination Formed by High-Density Turbidity Currents.Journal of Sedimentary Research, 75(1):1-5. https://doi.org/10.2110/jsr.2005.001
      [15] Liu, G.H., Huang, Z.L., Jiang, Z.X., et al., 2015.The Characteristic and Reservoir Significance of Lamina in Shale from Yanchang Formation of Ordos Basin.Natural Gas Geoscience, 26(3):408-417 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/trqdqkx201503002
      [16] Liu, Q., You, H.T., Liu, J.Q., 2004.Methodology of Studying on Varved Lake Sediments and Its Significance.Quaternary Sciences, 24(6):683-694 (in Chinese with English abstract).
      [17] Liu, S.G., Wang, S.Y., Sun, W., et al., 2013.Characteristics of Black Shale in Wufeng Formation and Longmaxi Formation in Sichuan Basin and Its Peripheral Areas.Journal of Chengdu University of Technology(Science & Technology Edition), 40(6):621-639 (in Chinese with English abstract).
      [18] Lu, Y.B., Ma, Y.Q., Wang, Y.X., et al., 2017.The Sedimentary Response to the Major Geological Events and Lithofacies Characteristics of Wufeng Formation-Longmaxi Formation in the Upper Yangtze Area.Earth Science, 42(7):1169-1184 (in Chinese with English abstract). https://doi.org/10.3799/dqkx.2017.095
      [19] Milliken, K.L., Rudnicki, M., Awwiller, D.N., et al., 2013.Organic Matter-Hosted Pore System, Marcellus Formation(Devonian), Pennsylvania.AAPG Bulletin, 97(2):177-200. https://doi.org/10.1306/07231212048
      [20] O'Brien, N.R., 1990.Significance of Lamination in Toarcian(Lower Jurassic) Shales from Yorkshire, Great Britain.Sedimentary Geology, 67(1-2):25-34. https://doi.org/10.1016/0037-0738(90)90025-o
      [21] O'Brien, N.R., 1996.Shale Lamination and Sedimentary Processes.Geological Society, London, Special Publications, 116(1):23-36. https://doi.org/10.1144/gsl.sp.1996.116.01.04
      [22] Ross, D.J.K., Marc Bustin, R., 2009.The Importance of Shale Composition and Pore Structure upon Gas Storage Potential of Shale Gas Reservoirs.Marine and Petroleum Geology, 26(6):916-927. https://doi.org/10.1016/j.marpetgeo.2008.06.004
      [23] Shi, Z.S., Qiu, Z., Dong, D.Z., et al., 2018.Laminae Characteristics of Gas-Bearing Shale Fine-Grained Sediment of the Silurian Longmaxi Formation of Well Wuxi 2 in Sichuan Basin, SW China.Petroleum Exploration and Development, 45(2):339-348 (in Chinese with English abstract).
      [24] Slatt, R.M., O'Brien, N.R., 2011.Pore Types in the Barnett and Woodford Gas Shales:Contribution to Understanding Gas Storage and Migration Pathways in Fine-Grained Rocks.AAPG Bulletin, 95(12):2017-2030. https://doi.org/10.1306/03301110145
      [25] Sun, J., Luo, B., 2016.Structural Deformation and Its Influences on Gas Storage in Fuling Shale Gas Play, the Sichuan Basin.Oil & Gas Geology, 37(6):809-818 (in Chinese with English abstract).
      [26] Tang, X.L., Jiang, Z.X., Jiang, S., et al., 2016.Heterogeneous Nanoporosity of the Silurian Longmaxi Formation Shale Gas Reservoir in the Sichuan Basin Using the QEMSCAN, FIB-SEM, and Nano-CT Methods.Marine and Petroleum Geology, 78:99-109. https://doi.org/10.1016/j.marpetgeo.2016.09.010
      [27] Walker, D., Owen, J.A.K., 1999.The Characteristics and Source of Laminated Mud at Lake Barrine, Northeast Australia.Quaternary Science Reviews, 18(14):1597-1624. https://doi.org/10.1016/s0277-3791(98)00119-x
      [28] Wang, C., Zhang, B.Q., Lu, Y.C., et al., 2018a.Lithofacies Distribution Characteristics and Main Development Controlling Factors of Shale in Wufeng Formation-Member 1 of Longmaxi Formation in Jiaoshiba Area.Acta Petrolei Sinica, 39(6):631-644 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/syxb201806003
      [29] Wang, C., Zhang, B.Q., Shu, Z.G., et al., 2018b.Lithofacies Types and Reservoir Characteristics of Marine Shales of the Wufeng Formation-Longmaxi Formation in Fuling Area, the Sichuan Basin.Oil & Gas Geology, 39(3):485-497 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/syytrqdz201803006
      [30] Wang, G.M., 2012.Laminae Combination and Genetic Classification of Eogene Shale in Jiyang Depression.Journal of Jilin University(Earth Science Edition), 42(3):666-671, 680 (in Chinese with English abstract).
      [31] Wang, G.M., Zhong, J.H., 2004.A Review and the Prospects of the Researches on Sedimentary Mechanism of Lacustrine Laminae.Acta Petrologica et Mineralogica, 23(1):43-48 (in Chinese with English abstract).
      [32] Wang, Y.M., Dong, D.Z., Li, X.J., et al., 2015.Stratigraphic Sequence and Sedimentary Characteristics of Lower Silurian Longmaxi Formation in the Sichuan Basin and Its Peripheral Areas.Natural Gas Industry, 35(3):12-21 (in Chinese with English abstract).
      [33] Xie, X.N., Hao, F., Lu, Y.C., et al., 2017.Differential Enrichment Mechanism and Key Technology of Shale Gas in Complex Areas of South China.Earth Science, 42(7):1045-1056 (in Chinese with English abstract). https://doi.org/10.3799/dqkx.2017.084
      [34] Yang, X., Jiang, C.F., Sun, B.H., et al., 2015.The Sandy Laminar Characteristics and Its Effect on Reservoir Property of Shale:A Case Study from the Upper Triassic Yanchang Fm in Southern Ordos Basin.Journal of Yanan University(Natural Science Edition), 34(2):18-23 (in Chinese with English abstract).
      [35] Yawar, Z., Schieber, J., 2017.On the Origin of Silt Laminae in Laminated Shales.Sedimentary Geology, 360:22-34. https://doi.org/10.1016/j.sedgeo.2017.09.001
      [36] Yi, J.Z., Wang, C., 2018.Differential Pore Development Characteristics in Various Shale Lithofacies of Longmaxi Formation in Jiaoshiba Area, Sichuan Basin.Petroleum Geology & Experiment, 40(1):13-19 (in Chinese with English abstract).
      [37] Zhao, J.H., Jin, Z.J., Jin, Z.K., et al., 2016.Lithofacies Types and Sedimentary Environment of Shale in Wufeng-Longmaxi Formation, Sichuan Basin.Acta Petrolei Sinica, 37(5):572-586 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/syytrqdz201803006
      [38] 程明, 罗晓容, 雷裕红, 等, 2015.鄂尔多斯盆地张家滩页岩粉砂质夹层/纹层分布、分形特征和估算方法研究.天然气地球科学, 26(5):845-854. http://www.cnki.com.cn/Article/CJFDTOTAL-TDKX201505008.htm
      [39] 郭彤楼, 2016.中国式页岩气关键地质问题与成藏富集主控因素.石油勘探与开发, 43(3):317-326. http://d.old.wanfangdata.com.cn/Periodical/syktykf201603001
      [40] 何治亮, 聂海宽, 张钰莹, 2016.四川盆地及其周缘奥陶系五峰组-志留系龙马溪组页岩气富集主控因素分析.地学前缘, 23(2):8-17. http://d.old.wanfangdata.com.cn/Periodical/dxqy201602002
      [41] 刘国恒, 黄志龙, 姜振学, 等, 2015.鄂尔多斯盆地延长组湖相页岩纹层发育特征及储集意义.天然气地球科学, 26(3):408-417. http://d.old.wanfangdata.com.cn/Periodical/trqdqkx201503002
      [42] 刘强, 游海涛, 刘嘉麒, 2004.湖泊沉积物年纹层的研究方法及其意义.第四纪研究, 24(6):683-694. doi: 10.3321/j.issn:1001-7410.2004.06.011
      [43] 刘树根, 王世玉, 孙玮, 等, 2013.四川盆地及其周缘五峰组-龙马溪组黑色页岩特征.成都理工大学学报(自然科学版), 40(6):621-639.
      [44] 陆扬博, 马义权, 王雨轩, 等, 2017.上扬子地区五峰组-龙马溪组主要地质事件及岩相沉积响应.地球科学, 42(7):1169-1184. https://doi.org/10.3799/dqkx.2017.095
      [45] 施振生, 邱振, 董大忠, 等, 2018.四川盆地巫溪2井龙马溪组含气页岩细粒沉积纹层特征.石油勘探与开发, 45(2):339-348. http://d.old.wanfangdata.com.cn/Periodical/syktykf201802018
      [46] 孙健, 罗兵, 2016.四川盆地涪陵页岩气田构造变形特征及对含气性的影响.石油与天然气地质, 37(6):809-818. http://d.old.wanfangdata.com.cn/Periodical/syytrqdz201606002
      [47] 王超, 张柏桥, 陆永潮, 等, 2018a.焦石坝地区五峰组-龙马溪组一段页岩岩相展布特征及发育主控因素.石油学报, 39(6):631-644. http://epub.cnki.net/grid2008/detail.aspx?filename=SYXB201806003&dbname=DKFX2018
      [48] 王超, 张柏桥, 舒志国, 等, 2018b.四川盆地涪陵地区五峰组-龙马溪组海相页岩岩相类型及储层特征.石油与天然气地质, 39(3):485-497. http://d.old.wanfangdata.com.cn/Periodical/syytrqdz201803006
      [49] 王冠民, 2012.济阳坳陷古近系页岩的纹层组合及成因分类.吉林大学学报(地球科学版), 42(3):666-671, 680. http://d.old.wanfangdata.com.cn/Periodical/cckjdxxb201203009
      [50] 王冠民, 钟建华, 2004.湖泊纹层的沉积机理研究评述与展望.岩石矿物学杂志, 23(1):43-48. doi: 10.3969/j.issn.1000-6524.2004.01.006
      [51] 王玉满, 董大忠, 李新景, 等, 2015.四川盆地及其周缘下志留统龙马溪组层序与沉积特征.天然气工业, 35(3):12-21. doi: 10.3787/j.issn.1000-0976.2015.03.002
      [52] 解习农, 郝芳, 陆永潮, 等, 2017.南方复杂地区页岩气差异富集机理及其关键技术.地球科学, 42(7):1045-1056. https://doi.org/10.3799/dqkx.2017.084
      [53] 杨潇, 姜呈馥, 孙兵华, 等, 2015.砂质纹层的发育特征及对页岩储层物性的影响——以鄂尔多斯盆地南部中生界延长组为例.延安大学学报(自然科学版), 34(2):18-23. http://d.old.wanfangdata.com.cn/Periodical/yadxxb201502005
      [54] 易积正, 王超, 2018.四川盆地焦石坝地区龙马溪组海相页岩储层非均质性特征.石油实验地质, 40(1):13-19. http://d.old.wanfangdata.com.cn/Periodical/sysydz201801002
      [55] 赵建华, 金之钧, 金振奎, 等, 2016.四川盆地五峰组-龙马溪组页岩岩相类型与沉积环境.石油学报, 37(5):572-586.
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