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辽河西部凹陷双南油田油气组成变化及成藏机制的地球化学分析

李虹 黄海平 史晓颖 马刊创

李虹, 黄海平, 史晓颖, 马刊创. 辽河西部凹陷双南油田油气组成变化及成藏机制的地球化学分析[J]. 石油实验地质, 2001, 23(4): 444-451. doi: 10.11781/sysydz200104444
引用本文: 李虹, 黄海平, 史晓颖, 马刊创. 辽河西部凹陷双南油田油气组成变化及成藏机制的地球化学分析[J]. 石油实验地质, 2001, 23(4): 444-451. doi: 10.11781/sysydz200104444
LI Hong, HUANG Hai-ping, SHI Xiao-ying, MA Kan-chuang. GEOCHEMICAL ANALYSES ON THE HYDROCARBON COMPOSITION CHANGES AND POOL-FORMING MECHANISMS OF SHUANGNAN OILFIELD IN THE WEST LIAOHE SAG[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2001, 23(4): 444-451. doi: 10.11781/sysydz200104444
Citation: LI Hong, HUANG Hai-ping, SHI Xiao-ying, MA Kan-chuang. GEOCHEMICAL ANALYSES ON THE HYDROCARBON COMPOSITION CHANGES AND POOL-FORMING MECHANISMS OF SHUANGNAN OILFIELD IN THE WEST LIAOHE SAG[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2001, 23(4): 444-451. doi: 10.11781/sysydz200104444

辽河西部凹陷双南油田油气组成变化及成藏机制的地球化学分析

doi: 10.11781/sysydz200104444
详细信息
    作者简介:

    李虹(1966- ),女(汉族),辽宁盘锦人,高级工程师,主要从事石油地质方面的研究工作.

  • 中图分类号: TE122.1

GEOCHEMICAL ANALYSES ON THE HYDROCARBON COMPOSITION CHANGES AND POOL-FORMING MECHANISMS OF SHUANGNAN OILFIELD IN THE WEST LIAOHE SAG

  • 摘要: 双南地区以产正常原油为主,并伴有少量的凝析油.观察发现,凝析油和正常油的总体特征(密度、粘度、含蜡量和凝固点)和某些生物标志化合物的含量变化较大.详细的地化分析表明,它们的成熟度相当.用多种分子标志物进行成熟度评估,可知液态烃的成熟度相当于Ro为0.7%~0.8%.这些原油有相同的生源构成,并形成于相似的沉积环境之中.原油总体组成和分子组成的变化归因于运移分馏过程,在该过程中气凝析油从与之相关的原油中分离出来,并运移到较浅的储层中聚集.认识运移分馏的过程和理解它在石油组分上的作用十分重要,因为许多用于油油、油源对比以及原油蚀变、油源类型和热成熟度等方面的地球化学指标都可能受到运移分馏作用的影响.

     

  • [1] Tissot B P,Welte D H.Petroleum Formation and Occurrence-A New Approach to Oil and Gas Exploration[M].Berlin:Springer,1984.
    [2] Snowdon L R,Powell T G.Immature oil and condensate-modification of hydrocarbon generation model for terrestrial organic matter[J].AAPG Bulletin,1982,66:775-788.
    [3] 卢松年,张刚.一种新的凝析油形成模式[J].中国科学(B辑),1994,24(1).
    [4] Gussow W C.Differential entrapment of oil and gas-a fundamental principle[J].AAPG Bulletin,1954,38:816-853.
    [5] Silverman S R.Migration and segregation of oil and gas[A].Yong A,Galley G E.Fluids in Subsurface Environments[C].AAPG Memoir,1965,4:53-65.
    [6] Thompson K F M.Fractionated aromatic petroleum and the ge-neration of gas-condensates[J].Org Geochem,1987,11(6):573-590.
    [7] Thompson K F M.Gas-condensate migration and oil fractionation in deltaic system[J].Mar Petrol Geol,1988,5:237-246.
    [8] Curiale J A,Bromley B W.Migration induced compositional change in oils and condensates of a single field[J].Org Geochem,1996,24(12):1 097-1 113.
    [9] Napitulu H,Ellis L,Mitterer R M.Post-generative alteration efforts on petroleum in the onshore Northwest Java Basin,Indonesia[J].Org Geochem,2000,31:295-315.
    [10] Dzou L I P,Hughes W B.Geochemistry of oils and condensates,K Field,offshore Taiwan:a case study in migration fractionation[J].Org Geochem,1993,20(4):437-462.
    [11] Khavari-Khorasani G,Dolson J C,Michlsen J K.The factors controlling the abundance and migration of heavy versus light oils,as constrained by data from the Gulf of Suez(Part I:the effect of expelled petroleum composition,PVT properties and petroleum system geometry)[J].Org Geochem,1998,29(1-3):255-282.
    [12] 葛泰生,陈义贤.中国石油地质志(卷三),辽河油田[M].北京:石油工业出版社,1993.
    [13] 张水昌.运移分馏作用:凝析油和蜡质油形成的一种重要机制.科学通报.2000,5(6):667-670.
    [14] Radke M.Application of aromatic compounds as maturity indicators in source rocks and crude oils[J].Mar Petrol Geol,1988,5:224-236.
    [15] Mello M R,Maxwell J R.Organic geochemical and biological marker characterization of source rocks and oils from lacustrine environments in the Brazilian Continental Margin[A].Katz B J.Lacustrine Basin Exploration[C].AAPG Memoir,1990,50:77-97.
    [16] Hughes W B,Holba A G,Dzou L I P.The ratios of dibenzo-thiophene to phenanthrene and pristane to phytane as indicators of depositional environment and lithology of petroleum source rocks[J].Geochimica et Cosmochimica Acta,1995,59:3 581-3 598.
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出版历程
  • 收稿日期:  2000-08-14
  • 修回日期:  2001-10-10
  • 刊出日期:  2001-10-25

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