Wu Yuyuan, Zan Ling, Huang Junping, Liu Chiyang, Feng Rujin, Qin Liming, Zhang Zhihuan. DISTRIBUTION CHARACTERISTICS AND GENESIS OF CO2 IN THE LAOYINGTAI-DAERHAN UPLIFT, THE CHANGLING FAULT SAG, THE SONGLIAO BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2009, 31(3): 237-243. doi: 10.11781/sysydz200903237
Citation: Wu Yuyuan, Zan Ling, Huang Junping, Liu Chiyang, Feng Rujin, Qin Liming, Zhang Zhihuan. DISTRIBUTION CHARACTERISTICS AND GENESIS OF CO2 IN THE LAOYINGTAI-DAERHAN UPLIFT, THE CHANGLING FAULT SAG, THE SONGLIAO BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2009, 31(3): 237-243. doi: 10.11781/sysydz200903237

DISTRIBUTION CHARACTERISTICS AND GENESIS OF CO2 IN THE LAOYINGTAI-DAERHAN UPLIFT, THE CHANGLING FAULT SAG, THE SONGLIAO BASIN

doi: 10.11781/sysydz200903237
  • Received Date: 2009-02-25
  • Rev Recd Date: 2009-04-09
  • Publish Date: 2009-06-28
  • CO2 gas or CO2 accompanied with hydrocarbon gas is widely distributed in the Laoyingtai Uplift of the Changling Fault Sag,the Songliao Basin.Contents and compositions of CO2 are different.Relative contents of CO2 and isotopic compositions may be obviously different between different wells or different gas formations in the same well,indicating complicate genesis.Studies of genetic mechanism of CO2 are important not only in theory,but also for natural gas exploration in the region.Based on CO2 composition and isotopic distribution features,combined with hydrocarbon gas studies,CO2 deep in the study area is both organic and inorganic origin,or mixed.CO2 in the Yingcheng Formation which contains much CO2 is mainly inorganic origin.CO2 in the Denglouku Formation which contains little CO2 is organic origin or mixed.Organic origin CO2 in the Denglouku Formation accumulates at the same time with hydrocarbon gas.Part of CO2 in the Yingcheng Formation accumulates at the same time with hydrocarbon gas;however,large accumulations of inorganic origin CO2 take place after Neogene.

     

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  • [1]
    米敬奎,张水昌,陶士振等.松辽盆地南部长岭断陷CO2 成因与成藏期研究[J].天然气地球科学,2008,19(4):452~456
    [2]
    谈迎,刘德良,李振生.松辽盆地北部二氧化碳气藏成因地球化学研究[J].石油实验地质,2006,28(5):480~488
    [3]
    霍秋立,付丽,王雪.松辽盆地北部CO2及He气成因与分布[J].大庆石油地质与开发,2004,23(4):1~4
    [4]
    杨会东,姚萍,张旭.松辽盆地南部无机成因CO2 成藏机制研究[J].天然气地球科学,2008,19(5):634~638
    [5]
    杨晓勇,刘德良,王佰长等.无机成因二氧化碳气成藏研究[J].石油实验地质,2007,29(2):154~161
    [6]
    周荔青,金之钧.松辽盆地无机成因气藏形成分布特征及勘探方向[J].石油实验地质,2009,31(1):12~18
    [7]
    付广,杨勉.松辽盆地北部天然气成藏与分布的主控因素[J].油气地质与采收率,2001,8(6):28~31
    [8]
    戴金星.各类烷烃气的鉴别[J].中国科学(B辑),1992,22(2):185~193
    [9]
    Pankina R G.Origin of CO2 in petroleum gases(from the isotopic composition of carbon)[J].International Geology Reviews,1978,21:535~539
    [10]
    李洪革,林心玉.长岭断陷深层构造特征及天然气勘探潜力分析[J].石油地球物理勘探,2006,41(9):33~36
    [11]
    周荔青,吴聿元,张淮.松辽盆地断陷层系油气成藏的分区特征[J].石油实验地质,2007,29(1):7~12
    [12]
    李春光.试论松辽盆地深层油气藏分布与形成[J].油气地质与采收率,2004,11(3):31~33
    [13]
    李本武,陈宪良.松原市区域基底构造特征及演化分析[J].东北地震研究,1999,15(2):51~57
    [14]
    陆建林,王果寿,朱建辉等.长岭凹陷深层成藏主控因素及勘探方向分析[J].石油天然气学报,2006,28(3):26~28
    [15]
    吴聿元,周荔青.松辽盆地主要断陷大中型油气田形成分布特征[J].石油实验地质,2007,29(3):231~237
    [16]
    吴群,周荔青.松辽盆地长岭断陷东部大中型火山岩(油)气田形成分布特征[J].石油实验地质,2009,31(1):40~45
    [17]
    刘成林,金惠,高嘉玉等.松辽盆地深层天然气成藏研究[J].油气地质与采收率,2009,16(1):1~4
    [18]
    秦伟军,刘超英,谈风其等.松辽盆地长岭断陷火山岩相与天然气成藏关系[J].石油实验地质,2008,30(4):328~332
    [19]
    刘福春.松辽盆地长岭凹陷南部成藏规律研究[D] :[学位论文].长春:吉林大学,2007
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