Shen Baojian, Yang Yunfeng, Tenger, Qin Jianzhong, Pan Anyang. Characteristics and hydrocarbon significance of organic matter in shale from the Jiaoshiba structure, Sichuan Basin: A case study of the Wufeng-Longmaxi formations in well Jiaoye1[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2016, 38(4): 480-488. doi: 10.11781/sysydz201604480
Citation: Shen Baojian, Yang Yunfeng, Tenger, Qin Jianzhong, Pan Anyang. Characteristics and hydrocarbon significance of organic matter in shale from the Jiaoshiba structure, Sichuan Basin: A case study of the Wufeng-Longmaxi formations in well Jiaoye1[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2016, 38(4): 480-488. doi: 10.11781/sysydz201604480

Characteristics and hydrocarbon significance of organic matter in shale from the Jiaoshiba structure, Sichuan Basin: A case study of the Wufeng-Longmaxi formations in well Jiaoye1

doi: 10.11781/sysydz201604480
  • Received Date: 2016-02-05
  • Rev Recd Date: 2016-06-15
  • Publish Date: 2016-07-28
  • Organic-rich shale samples were collected from the Upper Ordovician Wufeng-Longmaxi formations in the Jiaoshiba structure in the Sichuan Basin to carry out rock, kerogen and micro-fossil analyses. The biological recognition and organic petrologic analysis of hydrocarbon generation were carried out, and the hydrocarbon potential was discussed. Hydrocarbon precursor organisms in the high-maturity or over-mature Wufeng-Longmaxi shale mainly included acritarchs, alginite (lamalginite and benthic algae) and zooclasts (graptolite, chitinozoan and spicule), which were the major components of formed organic matter. However, amorphous organic matter was the primary portion in the Wufeng-Longmaxi shale, and was dispersed in the mineral matrix as fined particles. Shale gas in Jiaoshiba area was derived from hydrogen-rich alginite and macromolecular lipid polymer in graptolite tracheids. Abundant amorphous organic matter, especially plenty of pore-filling fine-grained bitumen, indicated that the source rocks have high hydrocarbon potential, which could form large shale gas fields.

     

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  • [1]
    张春明,张维生,郭英海.川东南—黔北地区龙马溪组沉积环境及对烃源岩的影响[J].地学前缘,2012,19(1):136-145. Zhang Chunming,Zhang Weisheng,Guo Yinghai.Sedimentary environment and its effect on hydrocarbon source rocks of Longmaxi Formation in southeast Sichuan and northern Guizhou[J].Earth Science Frontiers,2012,19(1):136-145.
    [2]
    林婉,肖传桃,石文睿,等.焦石坝页岩气田龙马溪组—五峰组沉积相特征[J].四川地质学报,2015,35(4):517-521. Lin Wan,Xiao Chuantao,Shi Wenrui,et al.Sedimentary facies of the Longmaxi Formation-Wufeng Formations in the Jiaoshiba shale gas field[J].Acta Geologica Sichuan,2015,35(4):517-521.
    [3]
    王玉满,董大忠,李新景,等.四川盆地及其周缘下志留统龙马溪组层序与沉积特征[J].天然气工业,2015,35(3):12-21. Wang Yuman,Dong Dazhong,Li Xinjing,et al.Stratigraphic sequence and sedimentary characteristics of Lower Silurian Longmaxi Formation in the Sichuan Basin and its peripheral areas[J].Natural Gas Industry,2015,35(3):12-21.
    [4]
    王志峰,张元福,梁雪莉,等.四川盆地五峰组—龙马溪组不同水动力成因页岩岩相特征[J].石油学报,2014,35(4):623-632. Wang Zhifeng,Zhang Yuanfu,Liang Xueli,et al.Characteristics of shale lithofacies formed under different hydrodynamic conditions in the Wufeng-Longmaxi formation,Sichuan Basin[J].Acta Petrolei Sinica,2014,35(4):623-632.
    [5]
    陈旭,樊隽轩,张元动,等.五峰组及龙马溪组黑色页岩在扬子覆盖区内的划分与圈定[J].地层学杂志,2015,39(4):351-358. Chen Xu,Fan Junxuan,Zhang Yuandong,et al.Subdivision and delineation of the Wufeng and Lungmachi black shales in the subsurface areas of the Yangtze platform[J].Journal of Stratigraphy,2015,39(4):351-358.
    [6]
    王哲,李贤庆,张吉振,等.四川盆地不同区块龙马溪组页岩气地球化学特征对比[J].中国煤炭地质,2016,28(2):22-27. Wang Zhe,Li Xianqing,Zhang Jizhen,et al.Longmaxi Formation shale gas geochemical features comparison between different blocks in Sichuan Basin[J].Coal Geology of China,2016,28(2):22-27.
    [7]
    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.
    [8]
    李延钧,刘欢,张烈辉,等.四川盆地南部下古生界龙马溪组页岩气评价指标下限[J].中国科学(地球科学),2013,43(7):1088-1095. Li Yanjun,Liu Huan,Zhang Liehui,et al.Lower limits of evaluation parameters for the Lower Paleozoic Longmaxi shale gas in southern Sichuan Province[J].Science China(Earth Sciences),2013,56(5):710-717.
    [9]
    李艳芳,邵德勇,吕海刚,等.四川盆地五峰组—龙马溪组海相页岩元素地球化学特征与有机质富集的关系[J].石油学报,2015,36(12):1470-1483. Li Yanfang,Shao Deyong,Lv Haigang,et al.A relationship between elemental geochemical characteristics and organic matter enrichment in marine shale of Wufeng Formation-Longmaxi Formation,Sichuan Basin[J].Acta Petrolei Sinica,2015,36(12):1470-1483.
    [10]
    路菁,李军,武清钊,等.页岩油气储层有机碳含量测井评价方法研究及应用[J].科学技术与工程,2016,16(6):143-147. Lu Jing,Li Jun,Wu Qingzhao,et al.A study and an application on logging evaluation method of TOC in shale oil and gas reservoir[J].Science Technology and Engineering,2016,16(6):143-147.
    [11]
    王秀平,牟传龙,葛详英,等.川南及邻区龙马溪组黑色岩系矿物组分特征及评价[J].石油学报,2015,36(2):150-162. Wang Xiuping,Mou Chuanlong,Ge Xiangying,et al.Mineral component characteristics and evaluation of black rock series of Longmaxi Formation in southern Sichuan and its periphery[J].Acta Petrolei Sinica,2015,36(2):150-162.
    [12]
    刘树根,王世玉,孙玮,等.四川盆地及其周缘五峰组—龙马溪组黑色页岩特征[J].成都理工大学学报(自然科学版),2013,40(6):621-639. Liu Shugen,Wang Shiyu,Sun Wei,et al.Characteristics of black shale in Wufeng Formation and Longmaxi Formation in Sichuan Basin and its peripheral areas[J].Journal of Chengdu University of technology (Science & Technology Edition),2013,40(6):621-639.
    [13]
    王秀平,牟传龙,葛祥英,等.四川盆地南部及其周缘龙马溪组黏土矿物研究[J].天然气地球科学,2014,25(11):1781-1794. Wang Xiuping,Mou Chuanlong,Ge Xiangying,et al.Study on clay minerals in the Lower Silurian Longmaxi Formation in southern Sichuan Basin and its periphery[J].Natural Gas Geoscience,2014,25(11):1781-1794.
    [14]
    张正顺,胡沛青,沈娟,等.四川盆地志留系龙马溪组页岩矿物组成与有机质赋存状态[J].煤炭学报,2013,38(5):766-771. Zhang Zhengshun,Hu Peiqing,Shen Juan,et al.Mineral compositions and organic matter occurrence modes of Lower Silurian Longmaxi Formation of Sichuan Basin[J].Journal of China Coal Society,2013,38(5):766-771.
    [15]
    姜振学,唐相路,李卓,等.川东南地区龙马溪组页岩孔隙结构全孔径表征及其对含气性的控制[J].地学前缘,2016,23(2):126-134. Jiang Zhenxue,Tang Xianglu,Li Zhuo,et al.The whole-aperture pore structure characteristics and its effect on gas content of the Longmaxi Formation shale in the southeastern Sichuan Basin[J].Earth Science Frontiers,2016,23(2):126-134.
    [16]
    王燕,冯明刚,魏祥峰,等.涪陵气田焦石坝区块页岩气储层储集空间特征及其定量评价[J].海相油气地质,2016,21(1):29-34. Wang Yan,Feng Minggang,Wei Xiangfeng,et al.Reservoir space characteristics and quantitative evaluation of shale gas reservoir at Jiaoshiba area in Fuling gas field[J].Marine Origin Petroleum Geology,2016,21(1):29-34.
    [17]
    郭雪晶,何顺利,陈胜,等.基于纳米CT及数字岩心的页岩孔隙微观结构及分布特征研究[J].中国煤炭地质,2016,28(2):28-34. Guo Xuejing,He Shunli,Chen Sheng,et al.Research on microstructure of shale pores and distribution features based on Nano-CT scanning and digital core analysis[J].Coal Geology of China,2016,28(2):28-34.
    [18]
    陈尚斌,朱炎铭,王红岩,等.四川盆地南缘下志留统龙马溪组页岩气储层矿物成分特征及意义[J].石油学报,2011,32(5):775-782. Chen Shangbin,Zhu Yanming,Wang Hongyan,et al.Characteristics and significance of mineral compositions of Lower Silurian Longmaxi Formation shale gas reservoir in the southern margin of Sichuan Basin[J].Acta Petrolei Sinica,2011,32(5):775-782.
    [19]
    黄磊,申维.页岩气储层孔隙发育特征及主控因素分析:以上扬子地区龙马溪组为例[J].地学前缘,2015,22(1):374-385. Huang Lei,Shen Wei.Characteristics and controlling factors of the formation of pores of a shale gas reservoir:A case study from Longmaxi Formation of the Upper Yangtze region,China[J].Earth Science Frontiers,2015,22(1):374-385.
    [20]
    胡宗全,杜伟,彭勇民,等.页岩微观孔隙特征及源—储关系:以川东南地区五峰组—龙马溪组为例[J].石油与天然气地质,2015,36(6):1001-1008. Hu Zongquan,Du Wei,Peng Yongmin,et al.Microscopic pore characteristics and the source-reservoir relationship of shale[J].Oil & Gas Geology,2015,36(6):1001-1008.
    [21]
    朱炎铭,张寒,亢韦,等.中上扬子地区龙马溪组、筇竹寺组页岩有机质微孔缝特征:生物发育与孔隙网络[J].天然气地球科学,2015,26(8):1507-1515. Zhu Yanming,Zhang Han,Kang Wei,et al.Organic nanopores of Longmaxi and Qiongzhusi formations in the Upper Yangtze:Biological precursor and pore network[J].Natural Gas Geoscience,2015,26(8):1507-1515.
    [22]
    刘树根,马文辛,Luba J,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,Luba J,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.
    [23]
    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. Guo Xusheng.Rules of two-factor enrichment for marine shale gas in Southern China:Understanding from the Longmaxi Formation shale gas in Sichuan Basin and its surrounding area[J].Acta Geologica Sinica,2014,88(7):1209-1218.
    [24]
    何治亮,聂海宽,张钰莹.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[J].地学前缘,2016,23(2):8-17. He Zhiliang,Nie Haikuan,Zhang Yuying.The main factors of shale gas enrichment of Ordovician Wufeng Formation-Silurian Longmaxi Formation in the Sichuan Basin and its adjacent areas[J].Earth Science Frontiers,2016,23(2):8-17.
    [25]
    郭彤楼,刘若冰.复杂构造区高演化程度海相页岩气勘探突破的启示:以四川盆地东部盆缘JY1井为例[J].天然气地球科学,2013,24(4):643-651. Guo Tonglou,Liu Ruobing.Implications from marine shale gas exploration breakthrough in complicated structural area at high thermal stage:Taking Longmaxi Formation in well JY1 as an example[J].Natural Gas Geoscience,2013,24(4):643-651.
    [26]
    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.
    [27]
    Evitt W R.A discussion and proposals concerning fossil dinoflagellates,hystrichospheres,and acritarchs,II[J].Proceedings of the National Academy of Sciences of the United States of America,1963,49(3):298-302.
    [28]
    Link C M,Bustin R M,Goodarzi F.Petrology of graptolites and their utility as indices of thermal maturity in Lower Paleozoic strata in northern Yukon,Canada[J].International Journal of Coal Geology,1990,15(2):113-135.
    [29]
    Briggs D E G,Kear A J,Baas M,et al.Decay and composition of the hemichordate Rhabdopleura:Implications for the taphonomy of graptolites[J].Lethaia,1995,28(1):15-23.
    [30]
    Goodarzi F.Organic petrography of graptolite fragments from Turkey[J].Marine and Petroleum Geology,1984,1(3):202-210.
    [31]
    Goodarzi F.Reflected light microscopy of chitinozoan fragments[J].Marine and Petroleum Geology,1985,2(1):72-78.
    [32]
    秦建中,申宝剑,付小东,等.中国南方海相优质烃源岩超显微有机岩石学与生排烃潜力[J].石油与天然气地质,2010,31(6):826-837. Qin Jianzhong,Shen Baojian,Fu Xiaodong,et al.Ultramicroscopic organic petrology and potential of hydrocarbon generation and expulsion of quality marine source rocks in south China[J].Oil & Gas Geology,2010,31(6):826-837.
    [33]
    秦建中,陶国亮,腾格尔,等.南方海相优质页岩的成烃生物研究[J].石油实验地质,2010,32(3):262-269. Qin Jianzhong,Tao Guoliang,Tenger,et al.Hydrocarbon-forming organisms in excellent marine source rocks in south China[J].Petroleum Geology & Experiment,2010,32(3):262-269.
    [34]
    秦建中,申宝剑,陶国亮,等.优质烃源岩成烃生物与生烃能力动态评价[J].石油实验地质,2014,36(4):465-472. Qin Jianzhong,Shen Baojian,Tao Guoliang,et al.Hydrocarbon-forming organisms and dynamic evaluation of hydrocarbon generation capacity in excellent source rocks[J].Petroleum Geology & Experiment,2014,36(4):465-472.
    [35]
    Towe K M,Urbanek A.Collagen-like structures in Ordovician graptolite periderm[J].Nature,1972,237(5356):443-445.
    [36]
    Crowther P R,Rickards R B.Cortical bandages and the graptolite zooid[J].Geologica et Palaeontologica,1977,11:9-46.
    [37]
    Bustin R M,Link C,Goodarzi F.Optical properties and chemistry of graptolite periderm following laboratory simulated maturation[J].Organic Geochemistry,1989,14(4):355-364.
    [38]
    Gupta N S,Briggs D E G,Pancost R D.Molecular taphonomy of graptolites[J].Journal of the Geological Society,2006,163(6):897-900.
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