Yi Shiwei, Jiang Youlu, Fan Bingda, Xu Haoqing, Zheng Ronghua. NEOGENE PETROLEUM SOURCE AND CHARACTERISTIC OF PALEOGENE HYDROCARBON SOURCE ROCK IN THE RAOYANG SAG, BOHAI BAY BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2010, 32(5): 475-479. doi: 10.11781/sysydz201005475
Citation: Yi Shiwei, Jiang Youlu, Fan Bingda, Xu Haoqing, Zheng Ronghua. NEOGENE PETROLEUM SOURCE AND CHARACTERISTIC OF PALEOGENE HYDROCARBON SOURCE ROCK IN THE RAOYANG SAG, BOHAI BAY BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2010, 32(5): 475-479. doi: 10.11781/sysydz201005475

NEOGENE PETROLEUM SOURCE AND CHARACTERISTIC OF PALEOGENE HYDROCARBON SOURCE ROCK IN THE RAOYANG SAG, BOHAI BAY BASIN

doi: 10.11781/sysydz201005475
  • Received Date: 2009-12-03
  • Rev Recd Date: 2010-08-16
  • Publish Date: 2010-10-28
  • There are two source rock beds,the lower Es1 and Es3 Formation,in Raoyang Sag of the Bohai Bay Basin.The deposition center of the Raoyang Sag was moved from southeast to northwest during the Paleogene.Based on saturated hydrocarbons chromatography and chromatography—mass spectrometry analysis of crude oil and source rocks,the relationship between Neogene crude oil and Paleogene source rocks was studied in the Raoyang Sag.Research has shown that Neogene oil in the Raoyang Sag mainly came from the lower Es1 source rocks,with the character of the nearest transportation.Affected by the distribution of source rocks,maturity and structure,Neogene oil mainly came from lower Es1 source rocks in the near oil-generating trough.In Wuqiang—Yangwuzhai area,hydrocarbon source rocks are not in oil-generating stage,Neogene oil mainly came from special lithologic section of the upper Es3.Besides,there is a phenomenon of mixed-source oil in Maxi area,Neogene oil mainly came from the lower Es1 in Maxi trough,and some came from the upper Es3 source rocks.

     

  • loading
  • [1]
    邓运华.渤海湾盆地上第三系油藏形成与勘探[J].中国海上油气(地质),2000,14(3):163-167.
    [2]
    薛永安,王应斌,赵建臣.渤海上第三系油藏形成特征及规律分析[J].石油勘探与开发,2001,28(5):1-6.
    [3]
    蒋有录,卓勤功,谈玉明,等.富油凹陷不同洼陷烃源岩的热演化及生烃特征差异性[J].石油实验地质,2009,31(5):500-505.
    [4]
    王权,高吉宏,唐宏,等.冀中坳陷上第三系油气藏成藏条件及分布[J].中国海上油气(地质),2001,15(1):56-60.
    [5]
    王建,马顺平,罗强,等.渤海湾盆地饶阳凹陷烃源岩再认识与资源潜力分析[J].石油学报,2009,30(1)51-55.
    [6]
    梁狄刚,曾宪章,王雪平,等.冀中坳陷油气的生成[M].北京:石油工业出版社,2001:1-205.
    [7]
    米立军.新构造运动与渤海海域上第三系大型油气田[J].中国海上油气(地质),2001,15(1):21-28.
    [8]
    龚再升,王国纯.渤海新构造运动控制晚期油气成藏[J].石油学报,2001,22(2):1-7.
    [9]
    秦建中,王静,李欣,等.渤海湾盆地饶阳凹陷未熟-低熟油成烃成藏条件研究[J].石油实验地质,2003,25(增刊):566-572.
    [10]
    罗宪婴,赵宗举,孟元林.正构烷烃奇偶优势在油源对比中的应用:以塔里木盆地下古生界为例[J].石油实验地质,2007,29(1):74-77.
    [11]
    彼得斯KE,莫尔多万J M.生物标记化合物指南:古代沉积物和石油中分子化石的解释[M].姜乃煌,张水昌,林永汉,等译.北京:石油工业出版社,1995:80-146.
  • 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 (3596) PDF downloads(940) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return