Advanced Search
Volume 29 Issue 6
. 
Turn off MathJax
Article Contents
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2007  >  29(6): 598-603
Zhou Shuqing, Huang Haiping, Liu Yuming. GEOCHEMICAL CHARACTERISTICS OF THE CRUDE OIL IN THE LUXI SAG, THE KAILU BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2007, 29(6): 598-603. doi: 10.11781/sysydz200706598
Citation: Zhou Shuqing, Huang Haiping, Liu Yuming. GEOCHEMICAL CHARACTERISTICS OF THE CRUDE OIL IN THE LUXI SAG, THE KAILU BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2007, 29(6): 598-603. doi: 10.11781/sysydz200706598
shu

GEOCHEMICAL CHARACTERISTICS OF THE CRUDE OIL IN THE LUXI SAG, THE KAILU BASIN

doi: 10.11781/sysydz200706598

  • School of Energy Resources, Chinese University of Geosciences, Beijing 100083, China

  • Received Date: 2007-01-22
  • Rev Recd Date: 2007-10-29
  • Publish Date: 2007-11-28
    Abstract
  • The Luxi Sag is the area which has the highest exploration degree and the most oil and gas discoveries among the peripheral basins of Liaohe Basin.The crude oil maturity,the organic matter input and the depositional environment of Bao 1 Block and Bao 14 Block in the Luxi Sag have been studied based on the precise geochemical analysises of the crude oil samples.Many similar geochemical characteristics between the crude oils from Bao 1 Block and Bao 14 Block have been found,in Cluding:the Pr/Ph ratio is less than 0.6;the regular sterane distribution is dominated by C29-steranes;the tricy Clic/pentacy Clic terpane ratio is less than 0.15,with the content of tricy Clic terpane being obviously less than pentacy Clic terpane;the base peak of the tricy Clic terpane is C23 and that of the pentacy Clic terpanes is C30,with the Ts/Tm ratio ranging from 0.7 to 1.0 and certain amount of gamacerene.But some differences between the two blocks also exist.Bao 14 Block has a slightly higher maturity,the base peak of n-alkanes in Bao 1 Block is mostly characterized by C20,and that in Bao 14 Block is mostly characterized by C21;the ratio of C15-21/C22-28 in Bao 1 Block is higher than that in Bao 14 Block;and Bao 1 Block has higher gamacerene index,indicating that Bao 1 Block was deposited under a higher salinity environment.The hopane/sterane ratio in Bao 1 Block is lower,suggesting that the algae were rather developed and the higher salinity environment may suppress the bateria.

     

    • FullText(HTML)
  • loading
    • References(28)
  • [1]
    Seifert W K,Moldowan J M.Use of biological markers in petroleum exploration[A].In:Johns R B,ed.Methods in Geochemistry and Geophysics,Biological Markers in Sedimentary Re cord 24[C].Amsterdam:Elsevier,1986.261～290
    [2]
    Mackenzie A S.Application of biological markers in petroleum geochemistry[A].In:Brooks J,Welte D,eds.Advances in Petroleum Geochemistry I[C].London:Academic Press,1984.115～214
    [3]
    Seifert W K,Moldowan J M.Paleoreconstruction by biological markers[J].Geochimica et Cosmochimica Acta,1981,45:783～794
    [4]
    Moldowan J M,Fago F J,Carlson R M K,et al.Rearranged hopanes in sediments and petroleum[J].Geochimica et Cosmochimica Acta,1991,55:3333～3353
    [5]
    Mackenzie A S,Hoffmann C F,Maxwell J R.Molecular parameters of maturation in the Toarcian shales,Paris Basin,France III.Changes in aromatic steroid hydrocarbons[J].Geochimica et Cosmochimica Acta,1981,45:1345～1355
    [6]
    Peters K E,Moldowan J.M.The biomarker guide:interpreting molecular fossils in petroleum and ancient sediments[M].Englewood Cliffs:Prentice Hall,1993.1～363
    [7]
    Didyk B M,Simoneit B R T,Brassell S C,et al.Organic geochemical indicators of palaeoenvironmental conditions of sedimentation[J].Nature,1978,272:216～222
    [8]
    Peters K E,Moldowan J M,Schoell M,et al.Petroleum isotopic and biomarker composition related to source rock organic matter and depositional environment[J].Organic Geochemistry,1986,10:17～27
    [9]
    Hughes W B,Holba A G,Dzou L I P.The ratios of dibenzothiophene to phenanthrene and pristane to phytane as indicators of depositional environment and lithology of petroleum source rocks[J].Geochimica et Cosmochimica Acta,1995,59:3581～3598
    [10]
    ten Haven H L,de Leeuw J W,Sinninghe Damsté J S,et al.Application of biological markers in the recognition of palaeohypersaline environments[A].In:Kdts K,Fleet A J,Talbot M,eds.Lacustrine Petroleum Source-rocks,Geological Society Special Publication 40[C].London:Blackwell,1988.123～130
    [11]
    Volkman J K.Biological marker compounds as indicators of the depositional environments of petroleum source-rocks[A].In:Kdts K,Fleet A J,Talbot M,eds.Lacustrine Petroleum Source-rocks,Geological Society Special Publication 40[C].London:Blackwell,1988.103～121
    [12]
    Volkman J K,Barrett S M,Blackburn S I,et al.Microalgal biomarkers:A review of recent research developments[J].Organic Geochemistry,1998,29:1163～1179
    [13]
    Philp R P,Gilbert T D.Biomarker distribution in oils predominantly derived from terrigenous source material[J].Organic Geochemistry,1986,10:73～84
    [14]
    Mello M R,Telnaes N,Gaglianone P C,et al.Organic geochemical characterization of depositional paleoenvironments in Brazilian marginal basins[J].Organic Geochemistry,1988,13:31～46
    [15]
    Moldowan J M,Seifert W K,Gallegos E J.Relationship between petroleum composition and depositional environment of petroleum source-rocks[J].AAPG Bulletin,1985,69:1255～1268
    [16]
    Connan J.Biodegradation of crude oils in reservoirs[A].In:Brooks J,Welte D,eds.Advances in Petroleum Geochemistry I[C].London:Academic Press,1984.299～335
    [17]
    ten Haven H L,de Leeuw J W,Rullktter J,et al.Restricted utility of the pristane/phytane ratio as a palaeoenvironmental indicator[J].Nature,1987,330:641～643
    [18]
    Dahl J E P,Moldowan J M,Teerman S C,et al.Source-rock quality determination from oil biomarkers Ⅰ.A new geochemical technique[J].AAPG Bulletin,1994,78:1507～1526
    [19]
    Moldowan J M,Lee C Y,Sundararaman P,et al.Source correlation and maturity assessment of select oils and rocks from the Central Adriatic basin (Italy and Yugoslavia)[A].In:Moldowan J M,Albrecht P,Philp R P,eds.Biological Markers in Sediments and Petroleum[C].Englewood Cliffs:Prentice Hall,1992.370～401
    [20]
    Peters K E,Moldowan J M,McCaffrey M A,et al.Selective biodegradation of extended hopanes to 25-norhopanes in petroleum reservoirs:Insights from molecular mechanics[J].Organic Geochemistry,1996,24:765～783
    [21]
    Damsté J S,Kenig F,Koopmans M P,et al.Evidence of gammacerane as an indicator of water column stratification[J].Geochimica et Cosmochimica Acta,1995,59:1895～1900
    [22]
    Mello M R,Telnaes N,Gaglianone P C,et al.Organic geochemical characterization of depositional paleoenvironments in Brazilian marginal basins[J].Organic Geochemistry,1988,13:31～46
    [23]
    Peters K E,Moldowan J M.Effects of source,thermal maturity and biodegradation on the distribution and isomerization of homohopanes in petroleum[J].Organic Geochemistry,1991,17:47～61
    [24]
    Rohmer M,Bisseret P,Neunlist S.The hopanoids,prokaryotic triterpenoids and precursors of ubiquitous molecular fossils[A].In:Moldowan J M,Albrecht P,Philp R P,eds.Biological Markers in Sediments and Petroleum[C].Englewood Cliffs:Prentice Hall,1992.1～17
    [25]
    Farrimond P,Fox P A,Innes H E,et al.Bacterial sources of hopanoids in recent sediments:improving our understanding of ancient hopane biomarkers[J].Ancient Biomolecules,1998,2:147～166
    [26]
    Volkman J K,Barrett S M,Dunstan G A,et al.Sterol biomarkers for microalgae from the green algal Class prasinophyceae[J].Organic Geochemistry,1994,21:1211～1218
    [27]
    Huang Y,Meinschein W G.Sterols as ecological indicators[J].Geochimica et Cosmochimica Acta,1979,43:739～745
    [28]
    Obermajer M,Fowler M G,Snowdon L R.Depositional environment and oil generation in Ordovician source rocks from southwestern Ontario,Canada:Organic geochemical and petrological approach[J].AAPG Bulletin,1999,83:1426～1453
    • 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 (691) PDF downloads(373) 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