Luo Xianying, Zhao Zongju, Meng Yuanlin. THE APPLICATION OF N-ALKANE'S ODD-EVEN CARBON NUMBER PREDOMINANCE IN OIL-SOURCE ROCK CORRELATION——AN EXAMPLE OF THE LOWER PALEOZOIC IN TARIM BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2007, 29(1): 74-77. doi: 10.11781/sysydz200701074
Citation: Luo Xianying, Zhao Zongju, Meng Yuanlin. THE APPLICATION OF N-ALKANE'S ODD-EVEN CARBON NUMBER PREDOMINANCE IN OIL-SOURCE ROCK CORRELATION——AN EXAMPLE OF THE LOWER PALEOZOIC IN TARIM BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2007, 29(1): 74-77. doi: 10.11781/sysydz200701074

THE APPLICATION OF N-ALKANE'S ODD-EVEN CARBON NUMBER PREDOMINANCE IN OIL-SOURCE ROCK CORRELATION——AN EXAMPLE OF THE LOWER PALEOZOIC IN TARIM BASIN

doi: 10.11781/sysydz200701074
  • Received Date: 2006-02-13
  • Rev Recd Date: 2006-12-04
  • Publish Date: 2007-01-28
  • The composition and distribution of the carbon number of n-alkane can reflect the source of organic matters,sedimentary environment and maturity of organic matter.Comparision of the n-alkane's GC diagrams in Tazhong Low Uplift shows that odd-carbon predominance appears in the Upper Ordovician source rocks,and even-carbon predominance has taken on in Cambrian-Lower Ordovician source rocks.The result of oil-source rock correlation shows that the origin of oils in the fields of Well TZ 10-11-12 is the Upper Ordovician source rocks,and the oils of Well TZ 45 and Well TZ 162 are from CambrianLower Ordovician source rocks.And the strata corresponding to the crude oils with odd-even carbon number predominance is accorded with what the oil-source rock correlation shows.In a word,the characteristics of n-alkane's odd-even carbon number predominance can be as an effective method for oil-source rock correlation in Tazhong Low Uplift,Tarim Basin.

     

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  • [1]
    林金辉,伊海生,邹艳荣.藏北高原海陆相油页岩生物标志化合物对比研究[J].地球化学,2004,33(1):57~64
    [2]
    朱扬明,苏爱国,梁狄刚等.柴达木盆地咸湖相生油岩正构烷烃分布特征及其成因[J].地球化学,2003,32(2):117~123
    [3]
    张水昌,王飞宇,张保民等.塔里木盆地中上奥陶统油源层地球化学研究[J].石油学报,2000,21(6):23~28
    [4]
    王飞宇,边立曾,张水昌等.塔里木盆地奥陶系海相源岩中两类生烃母质[J].中国科学(D辑),2001,31(2):96~102
    [5]
    Fowler M G.The influence of gloeocapsomopha prisca on the organic geochemistry of oils and organic rich rocks of late Ordovician age from Canada[A].In:Schidlowski M,ed.Early organic evolution:implications for mineral and energy resources[M].Berlin:Springer-Verlag,1992.336~356
    [6]
    Wehe D H,Waples D.Uber die Bevorzugung geradzahliger n-alkane in sedimentgesteinen[J].Natur Wissenschaften,1973,60:516~517
    [7]
    Shimoyama A,Jones W D.Formation of alkanes from fatty acids in the presence of CaCO3[J].Geochim Cosmochim Acta,1972,36:87~91
    [8]
    王铁冠.我国一些地区原油与生油岩中某些沉积环境生物标志物初探[A].见:王铁冠.生物标志物地球化学研究[M].武汉:中国地质大学出版社,1990.55~65
    [9]
    邓宏文,钱凯.沉积地球化学与环境分析[M].兰州:甘肃科学技术出版社,1993.1~178
    [10]
    李守军.正烷烃、姥鲛烷与植烷对沉积环境的指示意义[J].石油大学学报(自然科学版),1999,23(5):14~16
    [11]
    Mello M R.Organic geochemical characterization of depositional palaeoenvironments of source rocks and oils in brazilian marginal basins[J].Organic Geochemistry,1988,13:31
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