Qin Jianzhong. STUDY ON THE PETROLEUM RESOURCE POTENTIAL IN THE QIANGTANG BASIN, QINGHAI-TIBET PLATEAU[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2006, 28(6): 566-573. doi: 10.11781/sysydz200606566
Citation: Qin Jianzhong. STUDY ON THE PETROLEUM RESOURCE POTENTIAL IN THE QIANGTANG BASIN, QINGHAI-TIBET PLATEAU[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2006, 28(6): 566-573. doi: 10.11781/sysydz200606566

STUDY ON THE PETROLEUM RESOURCE POTENTIAL IN THE QIANGTANG BASIN, QINGHAI-TIBET PLATEAU

doi: 10.11781/sysydz200606566
  • Received Date: 2006-03-23
  • Rev Recd Date: 2006-10-31
  • Publish Date: 2006-11-28
  • Combining researches on the hydrocarbon source rock sedimentary environment,organic facies,organic matter's maturation and hydrocarbon-generating history with the geologic conditions in the Qiangtang Basin,Qinghai-Tibet Plateau,it is considered that the Jurassic J2b-J2x play in the central Qiangtang Basin,especially in the central parts of the South and North Qiangtang Depression is the most favorable target for exploration of the large and middle light oil/gas field or condensate field.In this Jurassic J2b-J2x play,the abundance of organic matters in mud shale and limerock is relatively high,good hydrocarbon source rock develops,red algae organic facies and mixed organic facies are dominant,most of the hydrocarbon source rocks are hige-mature to over-mature,there are two hydrocarbon-generating processes,the quantities of hydrocarbons and lihgt oil/gas is large.The Triassic T3x play in the center of Qiangtang Basin,especially in the center of the North Qiangtang Depression is the most favorable target for exploration of the large or super-large gas field.In this Triassic T3x play,the abundance of organic matters in mud shale is high,good hydrocarbon source rock developed,red algae organic facies and mixed organic facies are dominant,hydrocarbon source rocks are over-mature,the total hydrocarbon-generating quantity is great.

     

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  • [1]
    赵政璋,李永铁,费宝生等.青藏高原羌塘盆地石油地质[M].北京:科学出版社,2000.1~398.
    [2]
    赵政璋,秦建中,许怀先等.青藏高原海相烃源岩的油气生成[M].北京:科学出版社,2000.1~634.
    [3]
    秦建中.青藏高原羌塘盆地中生界主要烃源层分布特征[J].石油实验地质,2006,28(2):134~141,146.
    [4]
    秦建中,金聚畅,刘宝泉.海相不同类型烃源岩有机质丰度热演化规律[J].石油与天然气地质,2005,26(2):177~184.
    [5]
    秦建中.青藏高原羌塘盆地有机相展布与成烃模式[J].石油实验地质,2006,28(3):264~270,275.
    [6]
    叶和飞,夏邦栋,刘池阳等.青藏高原大地构造特征及盆地演化[M].北京:科学出版社,2000.1~439.
    [7]
    秦建中.青藏高原羌塘盆地油源及运移过程[J].石油实验地质,2006,28(5):450~457.
    [8]
    秦建中.羌塘盆地有机质热演化与成烃史研究[J].石油实验地质,2006,28(4):350~358.
    [9]
    沈启明,郭祖军,纪有亮等.青藏高原中生界沉积相及油气储盖层特征[M].北京:科学出版社,2000.24~117.
    [10]
    秦建中.青藏高原羌塘盆地海相烃源层的沉积形成环境[J].石油实验地质,2006,28(1):8~14,20.
    [11]
    罗本家,戴国汉.羌塘盆地油气有利勘探区块[J].石油与天然气地质,1996,17(1):58~61.
    [12]
    穆青.藏北油气远景及勘探方向[J].石油实验地质,1992,14(2):142~151.
    [13]
    Sassen R,Moore C H,Meendsen F C.Distribution of hydrocarbon source potential in the Jurassic Smacoover Formation[J].Organic Geochemistry,1987,11(3):379~383.
    [14]
    Carmalt S W,St John B.Giant oil and gas fields[A].In:Halbouty M T ed.Future Petroleum Province of the World,AAPG Memoir 40[M].Tulsa:AAPG,1986.11~53.
    [15]
    Jones R W.Comparison of carbonate and shale source rocks[A].In:Palacas J G ed.Petroleum Geochemistry and Source Rock Potential of Carbonate Rocks,AAPG Studies in Geology 18[M].Tulsa:AAPG,1984.163~180
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