Wang Yongjian, Wang Yanbin, Zheng Yabin, Liu Guofeng. HYDROCARBON SOURCE ROCK EVOLUTION IN TAIZHOU FORMATION, THE GAOYOU SAG, THE NORTH JIANGSU BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2007, 29(4): 411-414. doi: 10.11781/sysydz200704411
Citation: Wang Yongjian, Wang Yanbin, Zheng Yabin, Liu Guofeng. HYDROCARBON SOURCE ROCK EVOLUTION IN TAIZHOU FORMATION, THE GAOYOU SAG, THE NORTH JIANGSU BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2007, 29(4): 411-414. doi: 10.11781/sysydz200704411

HYDROCARBON SOURCE ROCK EVOLUTION IN TAIZHOU FORMATION, THE GAOYOU SAG, THE NORTH JIANGSU BASIN

doi: 10.11781/sysydz200704411
  • Received Date: 2006-11-15
  • Rev Recd Date: 2007-06-14
  • Publish Date: 2007-07-28
  • Researches on burial,temperature,maturity and oil generation histories of hydrocarbon source rocks of Taizhou Formation in the Gaoyou Sag,the North Jiangsu Basin with basin modeling methods have indicated that,hydrocarbon source rocks of Tai2 Member have entered mature stage and Ro has reached 0.6% during the early Sanduo period.As stratigraphic burial depth increases,stratum temperature,source rock maturity and hydrocarbon generation ability also increase gradually.In the end of Sanduo period,stratigraphic burial depth,temperature and hydrocarbon source rock maturity have reached the maximum,3 000 m,110℃,0.8%,respectively.At the same time,oil generation also reaches the maximum,and oil generation content of Well Jiao1 in the east reaches 350 mg/g.So,Sanduo period is the main stage during which Tai2 Member source rock generates and discharges hydrocarbon.In addition,tectonic and fault activities are strong during Sanduo period and most traps are formed.Therefore,Sanduo period is also the favorable and main period for oil-and-gas migration and accumulation.

     

  • loading
  • [1]
    侯建国,林承焰,姚合法等.断陷盆地成藏动力系统特征与油气分布规律:以苏北盆地为例[J].中国海上油气,2004,16(6):361~364
    [2]
    刘小平,王俊芳,李洪波.苏北盆地高邮凹陷热演化史研究[J].石油天然气学报(江汉石油学院学报),2005,27(1):17~18
    [3]
    李月容.油气成藏动力学模拟现状与展望[J].石油实验地质,2006,28(1):78~82
    [4]
    徐健,熊学洲.苏北盆地高邮凹陷油气成藏特征研究[J].石油勘探与开发,2000,27(4):80~83
    [5]
    李亚辉.苏北盆地高邮凹陷构造转换带控油机制研究[J].石油实验地质,2006,28(2):109~112
    [6]
    张庆春.盆地模拟技术的发展现状与未来展望[J].石油实验地质,2001,23(3):312~315
    [7]
    Welte D H,Yukler M A.Petroleum origin and accumulation in basin evolution:a quantitative mode[J].AAPG Bull,1981,11:1387~1396
    [8]
    徐晨光,张金功.盆地与油气成藏模拟软件的发展趋势分析[J].西安石油学院学报(自然科学版),2001,16(3):17~20
    [9]
    Miall A D.Principles of sedimentary basin analysis[M].2nd ed.New York:Springer-Verlag,1990
    [10]
    杨立干,陆英,陈平原.高邮凹陷上下第三系之间地层剥蚀量的研究[J].石油天然气学报(江汉石油学院学报),2003,25(增刊):33~34
    [11]
    刘小平,杨立干,徐健.苏北盆地高邮凹陷始新统剥蚀厚度恢复[J].新疆石油地质,2004,25(2):128~130
    [12]
    陈安定.苏北第三系成熟演化指标与深度关系的3种模式[J].石油实验地质,2003,25(1):58~63
  • 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 (916) PDF downloads(326) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return