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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2018  >  40(1): 118-125
LIU Meng, LIU Chao, SHU Zhiheng, LU Yongchao, GU Qian, TAN Congwen, XU Xiang. Heterogeneity characteristics and controlling factors of black shale in Jiaoshiba, Fuling, Sichuan Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2018, 40(1): 118-125. doi: 10.11781/sysydz201801118
Citation: LIU Meng, LIU Chao, SHU Zhiheng, LU Yongchao, GU Qian, TAN Congwen, XU Xiang. Heterogeneity characteristics and controlling factors of black shale in Jiaoshiba, Fuling, Sichuan Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2018, 40(1): 118-125. doi: 10.11781/sysydz201801118
shu

Heterogeneity characteristics and controlling factors of black shale in Jiaoshiba, Fuling, Sichuan Basin

doi: 10.11781/sysydz201801118
  • 1.

    Jianghan Oilfield Company, SINOPEC, Qianjiang, Hubei 433124, China

  • 2. China University of Geosciences, Faculty of Earth Resources, Wuhan, Hubei 430074, China

  • 3. Chongqing Fuling Shale Gas Exploration and Development Company, SINOPEC, Chongqing 408014, China

  • Received Date: 2017-10-09
  • Rev Recd Date: 2017-12-05
  • Publish Date: 2018-01-28
    Abstract
  • The study of macroscopic and microscopic heterogeneity of shale is one of the core aspects of shale gas exploration and development. The black shale in Jiaoshiba area in Fuling of Sichuan Province can be divided into two third-level sequences and nine sub-layers. The macroscopic heterogeneity mainly shows as follows. Laminations decrease first and then increase from bottom to top, sandy bands first increase and then decrease, while pyrites gradually decrease. Graptolithina in the transgressive system tract is mainly diplograptus type, while those in the early and late high system tracts are mainly monograptus type. Graptolithina abundance gradually reduces from bottom to top. The microscopic heterogeneity mainly shows as follows. TOC content in the transgressive system tract is the highest, and then decreases upwards, while clay mineral content gradually increases from bottom to top. On the whole, three kinds of sedimentation, bio-current, isochronous flow and terrigenous source, jointly controlled the heterogeneity of black shale in the Jiaoshiba area.

     

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    • References(20)
  • [1]
    刘树根,马文辛,JANSA L,等.四川盆地东部地区下志留统龙马溪组页岩储层特征[J].岩石学报,2011,27(8):2239-2252. LIU Shugen,MA Wenxin,JANSA L,et al.Characteristics of the shale gas reservoir rocks in the Lower Silurian Longmaxi Formation,east Sichuan Basin,China[J].Acta Petrologica Sinica,2011,27(8):2239-2252.
    [2]
    LOUCKS R G,REED R M,RUPPEL S C,et al.Preliminary classification of matrix pores in mudrocks[J].Gulf Coast Association of Geological Societies Transactions,2010,60:435-441.
    [3]
    LOUCKS R G,REED R M,RUPPEL S C,et al.Spectrum of pore types and networks in mudrocks and a descriptive classification for matrix-related mudrock pores[J].AAPG Bulletin,2012,96(6):1071-1098.
    [4]
    魏志红,魏祥峰.页岩不同类型孔隙的含气性差异:以四川盆地焦石坝地区五峰组-龙马溪组为例[J].天然气工业,2014,34(6):37-41. WEI Zhihong,WEI Xiangfeng.Comparison of gas-bearing property between different pore types of shale:A case from the Upper Ordovician Wufeng and Longmaxi Fms in the Jiaoshiba area,Sichuan Basin[J].Natural Gas Industry,2014,34(6):37-41.
    [5]
    ROSS D J,BUSTIN R M.Shale gas potential of the Lower Jurassic Gordondale Member,northeastern British Columbia,Canada[J].Bulletin of Canadian Petroleum Geology,2007,55(1):51-75.
    [6]
    高岗,柳广弟,王绪龙,等.准噶尔盆地上三叠统泥页岩解析气特征[J].天然气地球科学,2013,24(6):1284-1289. GAO Gang,LIU Guangdi,WANG Xulong,et al.Characteristics of separated shale gas from the Upper Triassic of Junggar Basin[J].Natural Gas Geoscience,2013,24(6):1284-1289.
    [7]
    ZHANG T W,ELLIS G S,RUPPEL S C,et al.Effect of organic-matter type and thermal maturity on methane adsorption in shale-gas systems[J].Organic Geochemistry,2012,47:120-131.
    [8]
    HILL R J,JARVIE D M,ZUMBERGE J,et al.Oil and gas geochemistry and petroleum systems of the Fort Worth Basin[J].AAPG Bulletin,2007,91(4):445-473.
    [9]
    XIA Xinyu,TANG Yongchun.Isotope fractionation of methane during natural gas flow with coupled diffusion and adsorption/desorption[J].Geochimica et Cosmochimica Acta,2012,77:489-503.
    [10]
    张金川,金之钧,袁明生.页岩气成藏机理和分布[J].天然气工业,2004,24(7):15-18. ZHANG Jinchuan,JIN Zhijun,YUAN Mingsheng.Reservoiring mechanism of shale gas and its distribution[J].Natural Gas Industry,2004,24(7):15-18.
    [11]
    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. 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.
    [12]
    聂海宽,张金川,张培先,等.福特沃斯盆地Barnett页岩气藏特征及启示[J].地质科技情报,2009,28(2):87-93. NIE Haikuan,ZHANG Jinchuan,ZHANG Peixian,et al.Shale gas reservoir characteristics of Barnett shale gas reservoir in Fort Worth Basin[J].Geological Science and Technology Information,2009,28(2):87-93.
    [13]
    徐旭辉,郑伦举,马中良.泥页岩中有机质的赋存形态与油气形成[J].石油实验地质,2016,38(4):423-428. XU Xuhui,ZHENG Lunju,MA Zhongliang.Organic matter occurrence and hydrocarbon generation in shale[J].Petroleum Geology & Experiment,2016,38(4):423-428.
    [14]
    郭英海,赵迪斐.微观尺度海相页岩气储层微观非均质性研究[J].中国矿业大学学报,2015,4(2):250-257. GUO Yinghai,ZHAO Difei.Micro-scale marine shale gas reservoir microscopic heterogeneity research[J].Journal of Chinese Mining University,2015,4(2):250-257.
    [15]
    高波.四川盆地龙马溪组页岩气地球化学特征及其地质意义[J].天然气地球科学,2015,26(6):1173-1182. GAO Bo.Geochemical characteristics of shale gas from Lower Silurian Longmaxi Formation in the Sichuan Basin and its geological significance[J].Natural Gas Geoscience,2015,26(6):1173-1182.
    [16]
    焦淑静,韩辉,翁庆萍,等.页岩孔隙结构扫描电镜分析方法研究[J].电子显微学报,2012,31(5):432-436. JIAO Shujing,HAN Hui,WENG Qingping,et al.Scanning electron microscope analysis of porosity in shale[J].Journal of Chinese Electron Microscopy Society,2012,31(5):432-436.
    [17]
    吉利明,邱军利,夏燕青,等.常见黏土矿物电镜扫描微孔隙特征与甲烷吸附性[J].石油学报,2012,33(2):249-256. JI Liming,CHU Junli,XIA Yanqing,et al.Characteristics of micro-pore and adsorption of methane by electron microscopy of common clay minerals[J].Petroleum Journal,2012,33(2):249-256.
    [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. 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.
    [19]
    秦华,范小军,刘明,等.焦石坝地区龙马溪组页岩解吸气地球化学特征及地质意义[J].石油学报,2016,37(7):846-854. QIN Hua,FAN Xiaojun,LIU Ming,et al.Geochemical characte-ristics and geological significance of desorbed shale gas in Longmaxi Formation,Jiaoshiba area[J].Acta Petrolei Sinica,2016,37(7):846-854.
    [20]
    黄文明,刘树根,王国芝,等.四川盆地下古生界油气地质条件及气藏特征[J].天然气地球科学,2011,22(3):465-476. HUANG Wenming,LIU Shugen,WANG Guozhi,et al.Characteristics of hydrocarbon geologic conditions and gas reservoirs in Lower Paleozoic of Sichuan Basin[J].Natural Gas Geoscience,2011,22(3):465-476.
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