Zhou Luyang, Liu Huaishan, Jiang Jianqun, Jing Xiangchun. CHARACTERISTICS AND ORIGINS OF THE CRUDE OIL IN OULITUOZI AREA OF THE EAST SAG, THE LIAOHE BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2007, 29(5): 490-494. doi: 10.11781/sysydz200705490
Citation: Zhou Luyang, Liu Huaishan, Jiang Jianqun, Jing Xiangchun. CHARACTERISTICS AND ORIGINS OF THE CRUDE OIL IN OULITUOZI AREA OF THE EAST SAG, THE LIAOHE BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2007, 29(5): 490-494. doi: 10.11781/sysydz200705490

CHARACTERISTICS AND ORIGINS OF THE CRUDE OIL IN OULITUOZI AREA OF THE EAST SAG, THE LIAOHE BASIN

doi: 10.11781/sysydz200705490
  • Received Date: 2006-07-04
  • Rev Recd Date: 2007-08-30
  • Publish Date: 2007-09-28
  • Oil-oil meticulous correlation research shows that there exist both immature and mature oils in Oulituozi area of the Liaohe Basin,and the maturity level of these oils is generally lower than those in the other areas of the East Sag.The lower maturity level of the oils in Oulituozi area is reveald by the following aspects:the ratio of saturated to aromatic hydrocarbons is low(3.0),the values of the maturity parameters of biomarkers and the stable carbon isotope values of saturated hydrocarbons and aromatics(-26.00‰~-27.50‰ and -25.00‰~-26.50‰ respectively) are also lower respectively than those in the other areas of the East Sag.The characteristics of the isotope contours of various individual hydrocarbons also indicates that the maturity of the oil in Oulituozi area is low.The results of oil-source correlation research suggest that the crude oil in Oulituozi area comes from the dark mudstone layers of the middle and lower parts of the 3rd member of Shahejie Formation,and the results of biomarker research show that the thermal evolution degree of the source rocks in Oulituozi area is apparently lower than those in the other areas of the East Sag,which causes the low maturity of the crude oil in the area.

     

  • loading
  • [1]
    王启军,陈建瑜.油气地球化学[M].武汉:中国地质大学出版社,1988.1~327
    [2]
    黄第藩.我国石油地球化学和应用方面几个问题的探讨[J].石油与天然气地质,1984,5(4):305~314
    [3]
    黄绍甫.四环藿烷——8,14-开环藿烷系列的鉴定及其地化意义[A].见:中国石油学会石油地质委员会.有机地球化学和陆相生油[C],北京:石油工业出版社,1986.102~111
    [4]
    王铁冠,钟宁宁.中国低熟油的几种成因机制[J].沉积学报,1997,15(2):75~83
    [5]
    郑冰,高仁祥.塔里木盆地原油碳硫同位素特征及油源对比[J].石油实验地质,2006(3):281~285
    [6]
    段毅,王智平,张辉等.柴达木盆地原油烃类地球化学特征[J].石油实验地质,2004(4):359~364
    [7]
    张文正,裵戈.液态烃正构烷烃系列、姥鲛烷、植烷碳同位素初步研究[J].石油勘探与开发,1992,19(5):32~41
    [8]
    赵孟军,黄第藩,张水昌.原油单体烃的碳同位素组成研究[J].石油勘探与开发,1994,21(3):52~59
    [9]
    Freeman K H,Hayes J M,Trendel J M,et al.Evidence from carbon isotope measurements for diverse origins of sedimentary hydrocarbon[J].Nature,1990,343:254~255
    [10]
    陈振岩,李军生,张戈等.辽河坳陷火山岩与油气[J].石油勘探与开发,1996,23(3):2~5
  • 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

    Article Metrics

    Article views (1199) PDF downloads(278) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return