Advanced Search
Volume 28 Issue 5
. 
Turn off MathJax
Article Contents
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2006  >  28(5): 430-433
Fu Zhifang, Tang Dazhen, Xu Hao, Yang Fang. FORMING MECHANISM OF SLOPE-BREAK AND ITS CONTROL ON SYN-DEPOSITIONAL FAULT AND DEPOSITION IN HALFGRABEN SAG—A CASE STUDY OF THE NANGYANG SAG, THE NANXIANG BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2006, 28(5): 430-433. doi: 10.11781/sysydz200605430
Citation: Fu Zhifang, Tang Dazhen, Xu Hao, Yang Fang. FORMING MECHANISM OF SLOPE-BREAK AND ITS CONTROL ON SYN-DEPOSITIONAL FAULT AND DEPOSITION IN HALFGRABEN SAG—A CASE STUDY OF THE NANGYANG SAG, THE NANXIANG BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2006, 28(5): 430-433. doi: 10.11781/sysydz200605430
shu

FORMING MECHANISM OF SLOPE-BREAK AND ITS CONTROL ON SYN-DEPOSITIONAL FAULT AND DEPOSITION IN HALFGRABEN SAG—A CASE STUDY OF THE NANGYANG SAG, THE NANXIANG BASIN

doi: 10.11781/sysydz200605430

  • China University of Geosciences, Beijing 100083, China

  • Received Date: 2005-06-10
  • Rev Recd Date: 2006-07-18
  • Publish Date: 2006-09-28
    Abstract
  • The slope-break zone is a pivotal zone of depositional physiognomy.The listric normal faults in the south of Nanyang Sag glide on lumpy surface and result in the gentle wrenches of cap formation in the north,serving as the boundary between depositional regions.Syn-depositional faults and sedimentary facies changes mainly take place here.Certain slope-break zone types indicate the activities and distributions of syn-depositional faults and control sediment dispersal and sand body accumulation.During different stages of basin evolution,syn-depositional faults and sedimentary facies belts control the gene-ration of different traps.

     

    • FullText(HTML)
  • loading
    • References(7)
  • [1]
    林畅松,潘元林."构造坡折带"——断陷盆地层序分析和油气预测的重要概念[J].地球科学,2000,25(3):260～263
    [2]
    任建业,陆永潮,张青林.断陷盆地构造坡折带形成机制及其对层序发育样式的控制[J].地球科学,2004,29(5):596～603
    [3]
    付志方,张本书,昝新等.南阳凹陷层序地层学研究[J].石油物探,2004,43(3):283～286
    [4]
    宗国洪,冯有良,刘承华等.同沉积断裂带砂砾岩隐蔽油藏研究——以东营凹陷胜北断裂带为例[J].石油实验地质,2003,25(3):274～279
    [5]
    陈宝宁,王宝言.济阳坳陷陡坡带层序地层特征[J].油气地质与采收率,2005,12(6):22～24
    [6]
    吴向阳.苏北盆地高邮凹陷北斜坡西部油气运移研究[J].石油实验地质,2005,27(3):281～287
    [7]
    王英民,金武弟,刘书会等.断陷湖盆多级坡折带的成因类型、展布及其勘探意义[J].石油与天然气地质,2003,24(3):199～302
    • 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 (739) PDF downloads(333) 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