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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2018  >  40(4): 526-531
WANG Dandan, ZHANG Wenhao, LI Shizhen, ZHOU Xingui, LIU Weibin. Features and hydrocarbon potential of source rocks in the Hongdi 1 well, Hongmiaozi Basin, Liaoning province[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2018, 40(4): 526-531. doi: 10.11781/sysydz201804526
Citation: WANG Dandan, ZHANG Wenhao, LI Shizhen, ZHOU Xingui, LIU Weibin. Features and hydrocarbon potential of source rocks in the Hongdi 1 well, Hongmiaozi Basin, Liaoning province[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2018, 40(4): 526-531. doi: 10.11781/sysydz201804526
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Features and hydrocarbon potential of source rocks in the Hongdi 1 well, Hongmiaozi Basin, Liaoning province

doi: 10.11781/sysydz201804526

  • Oil and Gas Survey, China Geological Survey, Beijing 100083, China

  • Received Date: 2018-03-02
  • Rev Recd Date: 2018-06-20
  • Publish Date: 2018-07-28
    Abstract
  • The Hongmiaozi Basin is one of the newly-identified Mesozoic sedimentary basins in the southeastern segment of the periphery of Songliao Basin. The degree of basic oil and gas geology research in the Hongmiaozi Basin is extremely low. The source rock types, organic geochemical features and hydrocarbon generation potential in the basin are unknown, which constrains the exploration and development of oil and gas resources in the basin. Based on the new drilling results of well Hongdi 1, some core samples were collected and tested for organic matter abundance, type and maturity of dark mudstone. The source rocks in the study area are mainly composed of black mudstone and silty mudstone in the Xiahuapidianzi Formation, Lower Cretaceous. The dark mudstone has a cumulative thickness of 101.16 m, and the single thickest layer is 24.85 m, finding fifty layers with oil and gas shows. The experimental results showed that source rocks of the Xiahuapidianzi Formation in the Hongmiaozi Basin have a medium organic matter abundance. The types of organic matter are mainly Ⅱ2-Ⅲ, partly Ⅱ1 and Ⅰ. The vitrinite reflectance ranges from 1.31% to 1.84%, with an average of 1.53%, indicating for a high maturity stage. Scanning electron micro-scopy analysis revealed that the mineral composition of source rocks consisted of clay and brittle minerals with average contents of 58.4% and 41.4%, respectively. Microporosity developed between muddy crystal grains, which is conducive to the improvement of storage space and migration channels, and to facilitate late artificial fracturing. The study showed that source rocks in the Hongmiaozi Basin have some potential for hydrocarbon generation, and there is an urgent need for continuous and intensive research.

     

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    • References(23)
  • [1]
    任纪舜,姜春发,张正坤,等.中国大地构造及其演化[M].北京:科学出版社,1980. REN Jishun,JIANG Chunfa,ZHANG Zhengkun,et al.Geotectonic evolution of China[M].Binjing:Science Press,1980.
    [2]
    方如恒.辽宁地质构造基本特征[J].辽宁地质,1985(3):189-200. FANG Ruheng.The fundamentai characteristics of geological structure in Liaoning province[J].Liaoning Geology,1985(3):189-200.
    [3]
    王声喜,苏永东,赵永利,等.辽宁抚顺地区金矿成矿地质条件及找矿方向探讨[J].矿物岩石,2008,28(1):39-47.

    WANG Shengxi,SU Yongdong,ZHAO Yongli,et al.Discussion on the metallogenic condition and ore-hunting criteria of gold in the Fushun area,Liaoning province[J].Journal of Mineralogy and Petrology,2008,28(1):39-47.
    [4]
    吉林省地质矿产局.吉林省区域地质志[M].北京:地质出版社,1988:208-209. Bureau of Geology and Mineral Resources of Jilin Province.Regional geology in Jinlin province[M].Beijing:Geological Publishing House,1988:208-209.
    [5]
    WANG Dandan,ZHOU Xingui,LI Shizhen,et al.New progress of oil and gas research in the Tonghua area,east of the Songliao Basin[J].Acta Geologica Sinica (English Edition),2017,91(4):1507-1508.
    [6]
    朱传玲,闫华,云露,等.塔里木盆地沙雅隆起星火1井寒武系烃源岩特征[J].石油实验地质,2014,36(5):626-632.

    ZHU Chuanling,YAN Hua,YUN Lu,et al.Characteristics of Cambrian source rocks in well XH1,Shaya Uplift,Tarim Basin[J].Petroleum Geology & Experiment,2014,36(5):626-632.
    [7]
    杨克明.四川盆地西部中三叠统雷口坡组烃源岩生烃潜力分析[J].石油实验地质,2016,38(3):366-374.

    YANG Keming.Hydrocarbon potential of source rocks in the Middle Triassic Leikoupo Formation in the Western Sichuan Depression[J].Petroleum Geology & Experiment,2016,38(3):366-374.
    [8]
    王安发,徐国盛,叶斌.石油及天然气地质学[M].成都:成都理工大学出版社,2002:105-115. WANG Anfa,XU Guosheng,YE Bin.Geology of oil and gas[M].Chengdu:Chengdu University of Technology Press,2002:105-115.
    [9]
    陈善斌,甘华军,时阳,等.北部湾盆地福山凹陷烃源岩地球化学特征及地质意义[J].油气地质与采收率,2015,22(1):14-19.

    CHEN Shanbin,GAN Huajun,SHI Yang,et al.Geochemical features and geologic significance of source rocks in Fushan Sag,Beibuwan Basin[J].Petroleum Geology and Recovery Efficiency,2015,22(1):14-19.
    [10]
    张洪安,徐田武,张云献.东濮凹陷咸化湖盆优质烃源岩的发育特征及意义[J].断块油气田,2017,24(4):437-441.

    ZHANG Hongan,XU Tianwu,ZHANG Yunxian.Development characteristics and significance of high quality source rocks of salty lake in Dongpu Depression[J].Fault-Block Oil and Gas Field,2017,24(4):437-441.
    [11]
    曲彦胜,王圣,李艳丽,等.乌伦古地区石炭系烃源岩生烃潜力评价[J].特种油气藏,2016,23(2):31-35.

    QU Yansheng,WANG Shengzhu,LI Yanli,et al.Hydrocarbon potential evaluation of carboniferous source-rocks in Wulungu[J].Special Oil & Gas Reservoirs,2016,23(2):31-35.
    [12]
    袁东山,郜建军,朱建辉,等.鄂尔多斯富县地区下古生界烃源岩地球化学特征[J].石油天然气学报,2009,31(4):58-62.

    YUAN Dongshan,GAO Jianjun,ZHU Jianhui,et al.Geochemical characteristics of Lower Palaeozoic hydrocarbon source rocks in Fuxian exploration area of Ordos Basin[J].Journal of Oil and Gas Technology,2009,31(4):58-62.
    [13]
    党犇,赵虹,姜常义.塔里木盆地东北部侏罗系烃源岩特征及初步评价[J].地球科学与环境学报,2004,26(1):1-5.

    DANG Ben,ZHAO Hong,JIANG Changyi.Preliminary studies and characteristics of the Jurassic hydrocarbon source rocks in the northern Tarim Basin[J].Journal of Earth Sciences and Environment,2004,26(1):1-5.
    [14]
    腾格尔,秦建中,付小东,等.川东北地区上二叠统吴家坪组烃源岩评价[J].古地理学报,2010,12(3):334-346.

    TENGER Boltsjin,QIN Jianzhong,FU Xiaodong,et al.Hydrocarbon source rocks evaluation of the Upper Permian Wujiaping Formation in northeastern Sichuan area[J].Journal of Palaeogeography,2010,12(3):334-346.
    [15]
    中原石油勘探局勘探开发研究院. 陆相烃源岩地球化学评价方法:SY/T 5735-1995[S].北京:石油工业出版社,1996:1-19. Research Institute of Exploration and Development of Zhongyuan Petroleum Exploration Bureau.Geochemical evaluation method of continental-facies source rock:SY/T5735-1995[S].Beijing:Petroleum Industry Press,1995:1-19.
    [16]
    秦建中.中国烃源岩[M].北京:科学出版社,2005. QIN Jianzhong.Source rocks of China[M].Binjing:Science Press,2005.
    [17]
    陈安定.海相"有效烃源岩"定义及丰度下限问题讨论[J].石油勘探与开发,2005,32(2):23-25.

    CHEN Anding.Definition and abundance threshold of marine source rocks developed in South China[J].Petroleum Exploration and Development,2005,32(2):23-25.
    [18]
    CHALMERS G R L,BUSTIN R M.On the effects of petrographic composition on coalbed methane sorption[J].International Journal of Coal Geology,2007,69(4):288-304.
    [19]
    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.
    [20]
    吉利明,邱军利,张同伟,等.泥页岩主要黏土矿物组分甲烷吸附实验[J].地球科学(中国地质大学学报),2012,37(5):1043-1050. JI Liming,QIU Junli,ZHANG Tongwei,et al.Experiments on methane adsorption of common clay minerals in shale[J].Earth Science(Journal of China University of Geosciences),2012,37(5):1043-1050.
    [21]
    邹才能,杨智,崔景伟,等.页岩油形成机制、地质特征及发展对策[J].石油勘探与开发,2013,40(1):14-26.

    ZOU Caineng,YANG Zhi,CUI Jingwei,et al.Formation mechanism,geological characteristics and development strategy of non-marine shale oil in China[J].Petroleum Exploration and Development,2013,40(1):14-26.
    [22]
    耳闯,赵靖舟,白玉斌,等.鄂尔多斯盆地三叠系延长组富有机质泥页岩储层特征[J].石油与天然气地质,2013,34(5):708-716.

    ER Chuang,ZHAO Jingzhou,BAI Yubin,et al.Reservoir characte-ristics of the organic-rich shales of the Triassic Yanchang Formation in Ordos Basin[J].Oil & Gas Geology,2013,34(5):708-716.
    [23]
    王丹丹,周新桂,李世臻,等.通化盆地下白垩统烃源岩石油地质特征及生烃潜力研究[J].地质学报,2017,91(9):2119-2130.

    WANG Dandan,ZHOU Xingui,LI Shizhen,et al.Petroleum geologic features and generation potential of the Lower Cretaceous hydrocarbon source rocks in the Tonghua Basin[J].Acta Geologica Sinica,2017,91(9):2119-2130.
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