Advanced Search
Volume 35 Issue 2
. 
Turn off MathJax
Article Contents
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2013  >  35(2): 179-186
Qin Jianzhong, Shen Baojian, Tenger, Zheng Lunju, Tao Guoliang, Fu Xiaodong, Zhang Linglong. Hydrocarbon generation and expulsion pattern of different types of excellent source rocks[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2013, 35(2): 179-186. doi: 10.11781/sysydz201302179
Citation: Qin Jianzhong, Shen Baojian, Tenger, Zheng Lunju, Tao Guoliang, Fu Xiaodong, Zhang Linglong. Hydrocarbon generation and expulsion pattern of different types of excellent source rocks[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2013, 35(2): 179-186. doi: 10.11781/sysydz201302179
shu

Hydrocarbon generation and expulsion pattern of different types of excellent source rocks

doi: 10.11781/sysydz201302179
  • 1.

    Wuxi Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214126, China

  • 2. SINOPEC Key Laboratory for Petroleum Accumulation Mechanisms, Wuxi, Jiangsu 214126, China

  • Received Date: 2012-11-09
  • Rev Recd Date: 2013-01-25
  • Publish Date: 2013-03-28
    Abstract
  • Semi-closed pyrolysis experiments were conducted in order to evaluate what controls the hydrocarbon generation and expulsion efficiency for three types of excellent source rocks (siliceous, calcareous and clay ones). Each type of source rock has different relative hydrocarbon expulsion efficiencies in the stage of early-middle oil window, where siliceous source rock has the highest oil expulsion efficiency and oil expulsion quantity, reaching to 50%, and the expelled products are dominated by heavy oil. This is followed by calcareous source rock, about 30%. The oil expulsion efficiency of clay source rock is the lowest, about 4%-11%. During the middle-late maturation stage, siliceous source rock tends to achieve the highest expulsion efficiency first, followed by calcareous source rock (65%) and then clay source rock. During the late and high-mature stage, the oil expulsion efficiencies of siliceous and calcareous source rocks do not change obviously, while the oil expulsion efficiency of clay source rock increases rapidly from 20% to 90%. The models of hydrocarbon generation and expulsion of three types of excellent source rocks are different in the stage of early-middle oil window.

     

    • FullText(HTML)
  • loading
    • References(33)
  • [1]
    张林晔. 湖相烃源岩研究进展[J].石油实验地质,2008,30(6):591-595.
    [2]
    秦建中,腾格尔,付小东.海相优质烃源层评价与形成条件研究[J].石油实验地质,2009,31(4):366-372.
    [3]
    吴亚生,钟大康,邱楠生,等.松南地区断陷层烃源岩生烃能力及主控因素分析[J].断块油气田,2012,19(1):39-43.
    [4]
    腾格尔.中国海相烃源岩研究进展及面临的挑战[J].天然气工业,2011,31(1):20-25.
    [5]
    Clegg H,Wilkes H,Horsfield B.Carbazole distributions in carbonate and clastic source rocks[J].Geochimica et Cosmochimica Acta,1997,61:5335-5345.
    [6]
    陈义才,沈忠民,罗小平.石油与天然气有机地球化学[M].北京:科学出版社,2007:56-58.
    [7]
    Riboulleau A,Baudin F,Deconinck J F,et al.Depositional conditions and organic matter preservation pathways in an epicontinental environment:the Upper Jurassic Kashpir Oil Shales (Volga Basin,Russia)[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2003,197:171-197.
    [8]
    Yin H F,Xie S C,Yan J X,et al.Geobiological approach to evaluating marine carbonate source rocks of hydrocarbon[J].Sci China:Earth Sci,2011,54(8):1121-1135.
    [9]
    Glikson M.The application of electron microscopy and microanalysis in conjunction with organic petrology to further the understanding of organic-miner al association:Examples from Mount Isa and McArthur basins,Australia[J].International Journal of Coal Geology,2001, 47:139-159.
    [10]
    Younes M A,Philp R P.Source rock characterization based on biological marker distributions of crude oils in the southern Gulf of Suez,Egypt [J].Journal of Petroleum Geology,2005,28(3):301-317.
    [11]
    Ercegovac M,Kostic A.Organic facies and paly nofacies:Nomenclature,classification and applicability for petroleum source rock evaluation [J].International Journal of Coal Geology,2006,68:70-78.
    [12]
    母国妍,钟宁宁,刘宝,等.湖相泥质烃源岩的定量评价方法及其应用[J].石油学报,2010,31(2):218-224.
    [13]
    张水昌,梁狄刚,张大江.关于古生界烃源岩有机质丰度评价标准[J].石油勘探与开发,2002,29(2):8-12.
    [14]
    秦建中.中国烃源岩[M].北京:科学出版社,2005.
    [15]
    Vandenbroucke M,Largeau C.Kerogen origin,evolution and structure[J].Organic Geochemistry,2007,38:719-833.
    [16]
    秦建中,付小东,申宝剑,等.四川盆地上二叠统海相优质页岩超显微有机岩石学特征研究[J].石油实验地质,2010,32(2):164-170.
    [17]
    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.
    [18]
    陈洁,鹿坤,冯英,等.东濮凹陷不同环境烃源岩评价及生排烃特征研究[J].断块油气田,2012,19(1):35-38.
    [19]
    庞雄奇,李素梅,金之钧,等.排烃门限存在的地质地球化学证据及其应用[J].地球科学——中国地质大学学报,2004,29(4):384-390.
    [20]
    霍秋立,曾花森,乔万林,等.松辽盆地优质烃源岩含水生排油模拟实验[J].大庆石油地质与开发,2011,30(4):1-6.
    [21]
    秦建中,刘井旺,刘宝泉,等.加温时间、加水量对模拟实验油气产率及地化参数的影响[J].石油实验地质,2002,24(2):152-157.
    [22]
    李志明,秦建中,刘宝泉.柴达木盆地上第三系泥岩生烃热压模拟实验[J].天然气工业,2005,25(2):30-32.
    [23]
    蔡希源.湖相烃源岩生排烃机制及生排烃效率差异性:以渤海湾盆地东营凹陷为例[J].石油与天然气地质,2012,33(3):329-334.
    [24]
    辛艳朋,邱楠生,秦建中,等.塔里木盆地奥陶系烃源岩二次生烃研究[J].地球科学与环境学报,2011,33(3):261-267.
    [25]
    马行陟,庞雄奇,孟庆洋,等.辽东湾地区深层烃源岩排烃特征及资源潜力[J].石油与天然气地质,2011,32(2):251-258.
    [26]
    秦建中,刘宝泉,郑伦举.海相碳酸盐岩生排烃能力研究[J].石油与天然气地质,2006,27(3):348-355.
    [27]
    秦建中,刘宝泉.海相不同类型烃源岩生排烃模式研究[J].石油实验地质,2005,27(1):74-80.
    [28]
    江林香,王庆涛,卢鸿,等.开放体系下平凉组页岩干酪根的生烃动力学研究[J].地球化学,2012,41(2):139-146.
    [29]
    王云鹏,赵长毅,王兆云,等.利用生烃动力学方法确定海相有机质的主生气期及其初步应用[J].石油勘探与开发,2005,32(4):153-158.
    [30]
    蒋启贵,王延斌,秦建中,等.中国南方海相烃源岩生烃动力学研究[J].石油实验地质,2008,30(6):606-610.
    [31]
    Banerjee A,Jha M,Mittal A K,et al.The effective source rocks in the north Cambay Basin[J].Marine and Petroleum Geology,2000,17(10):1111-1129.
    [32]
    李志明,郑伦举,马中良,等.烃源岩有限空间油气生排模拟及其意义[J].石油实验地质,2011,33(5):447-451.
    [33]
    郑伦举,秦建中,何生,等.地层孔隙热压生排烃模拟实验初步研究[J].石油实验地质,2009,31(3):296-302,306.
    • Relative Articles
    • Supplements(0)
    • Cited By
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索
    Citation
    XML
    PDF-CN

    Article Metrics

    Article views (1853) PDF downloads(931) Cited by()
    Proportional views
    Related

    Website Copyright © Wuxi Research Institute of Petroleum Geology, SINOPEC 苏ICP备15009037号 苏公网安备32021102000780号

    Address：No. 2060, Lihu Avenue, Wuxi, Jiangsu   (214126) Tel：0510-68787204，68787203 Fax：0510-68787113 Email：sysydz.syky@sinopec.com

    Supported by: Beijing Renhe Information Technology Co. Ltd    

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return