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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2009  >  31(5): 506-511
Wang Jie, Liu Wenhui, Wang Tieguan, Chen Jianfa. SOURCE ROCK AND OIL GEOCHEMISTRY AND CORRELATION IN SHUANGCHENG-TAIPINGCHUAN AREA, THE SONGLIAO BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2009, 31(5): 506-511. doi: 10.11781/sysydz200905506
Citation: Wang Jie, Liu Wenhui, Wang Tieguan, Chen Jianfa. SOURCE ROCK AND OIL GEOCHEMISTRY AND CORRELATION IN SHUANGCHENG-TAIPINGCHUAN AREA, THE SONGLIAO BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2009, 31(5): 506-511. doi: 10.11781/sysydz200905506
shu

SOURCE ROCK AND OIL GEOCHEMISTRY AND CORRELATION IN SHUANGCHENG-TAIPINGCHUAN AREA, THE SONGLIAO BASIN

doi: 10.11781/sysydz200905506
  • 1.

    Wuxi Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214151, China

  • 2. Chinese University of Petroleum, Beijing 102249, China

  • Received Date: 2008-12-16
  • Rev Recd Date: 2009-08-24
  • Publish Date: 2009-09-28
    Abstract
  • Shuangcheng-Taipingchuan is an important petroleum exploration area in the north of Songliao Basin.By synthetically analyzing geochemical characteristics of petroleum and mudstone,it indicates that petroleum belongs to the same population in Fuyu and Yangdachengzi oil layer.The studied petroleum mainly comes from Qing 1 member and partly from Qing 2+3 member mudstone of the Sanzhao Sag and the Chaoyanggou Bench,but not from Nen 1 member mudstone.Moreover,oil of the Sanzhao Sag and the Chaoyanggou Bench mainly comes from their Qing 1 member hydrocarbon source kitchen.Petroleum of the Changchunling Anticline Belt and the Wangfu Sag mainly comes from Qing 1 member hydrocarbon source kitchen in the Wangfu Sag.Qing 1 member hydrocarbon source kitchen of the Sanzhao Sag and the Chaoyanggou Bench also has partial contribution to petroleum in the Changchunling Anticline Belt.

     

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    • References(9)
  • [1]
    高瑞琪,蔡希源.松辽盆地油气田形成条件与分布规律[M].北京:石油工业出版社,1997.10～101
    [2]
    王杰,王铁冠,陈践发等.松辽盆地双城-太平川地区原油地球化学特征及其成熟度差异[J].海相油气地质,2009,14(1):65～70
    [3]
    Galimov E M.13C/12C in kerogens[A].In:Durand B,ed.Insoluble organic matter from sedimentary rocks[C].Paris:Editions Technip,1980.271～299
    [4]
    吴河勇,李景坤.松辽盆地北部深层原油的碳同位素特征及成因探讨[J].石油实验地质,2003,25(3):300～304
    [5]
    Stahl W J.Carbon and nitrogen isotopes in hydrocarbon research and exploration[J].Chemical Geology,1977,20(2):1121～1149
    [6]
    郑冰,高仁祥.塔里木盆地原油碳硫同位素特征及油源对比[J].石油实验地质,2006,28(3):281～285
    [7]
    霍秋立,冯子辉,傅丽.王府凹陷油源与原油地球化学特征[J].大庆石油地质与开发,1996,15(4):22～25
    [8]
    王杰.松辽盆地双城-太平川地区油气地球化学特征及油气源对比研究[D].北京:国家图书馆,2005
    [9]
    郭少斌,刘招君,刘万洙等.应用特征分析法预测松辽盆地扶余油层有利勘探区[J].石油实验地质,1994,16(2):157～163
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