Advanced Search
Volume 35 Issue 4
. 
Turn off MathJax
Article Contents
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2013  >  35(4): 407-413
Wu Guoqiang, Lü Xiuxiang, Zhou Xinhuai, Yu Yixin, Tian Ya, Jiang Ziwen. Response of Cenozoic Tan-Lu fault activity in Laizhou Bay area, Bohai Sea[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2013, 35(4): 407-413. doi: 10.11781/sysydz201304407
Citation: Wu Guoqiang, Lü Xiuxiang, Zhou Xinhuai, Yu Yixin, Tian Ya, Jiang Ziwen. Response of Cenozoic Tan-Lu fault activity in Laizhou Bay area, Bohai Sea[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2013, 35(4): 407-413. doi: 10.11781/sysydz201304407
shu

Response of Cenozoic Tan-Lu fault activity in Laizhou Bay area, Bohai Sea

doi: 10.11781/sysydz201304407
  • 1.

    College of Geosciences, China University of Petroleum, Beijing 102249, China

  • 2. State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing 102249, China

  • 3. CNOOC Tianjin Branch Company, Tianjin 300452, China

  • Received Date: 2012-07-02
  • Rev Recd Date: 2013-05-07
  • Publish Date: 2013-07-28
    Abstract
  • By using the latest 3D seismic data, we described the space distribution of the Tan-Lu fault in the southern Bohai area and analyzed the evolution history and the influence to sedimentation and tarp formation combining the previous research achievements. The results showed that: in the southern Bohai area, flower structure and formation dag were revealed in the Tan-Lu fault and the salt activity was also a strong evidence for the strik-slip movement of the Tan-Lu fault in Cenozoic. The activity of the Tan-Lu fault had a significant impact on the evolution of the Laizhou Bay Sag, mainly reflected by the migration of sedimentary center. It also led to the formation of traps in both deep and shallow layers and most of the traps were faulted anticlines and fault blocks.

     

    • FullText(HTML)
  • loading
    • References(31)
  • [1]
    张鹏,王良书,石火生,等.郯庐断裂带山东段的中新生代构造演化特征[J].地质学报,2010,84(9):1316-1323.
    [2]
    许志琴.郯庐裂谷系概述[J].构造地质论丛,1984(3):39-46.
    [3]
    朱光,王道轩,刘国生,等.郯庐断裂带的演化及其对西太平洋板块运动的响应[J].地质科学,2004,39(1):36-49.
    [4]
    陈宣华,王小凤,张青,等.郯庐断裂带形成演化的年代学研究[J].长春科技大学学报,2000,30(3):215-220.
    [5]
    万天丰,朱鸿,赵磊,等.郯庐断裂带的形成与演化:综述[J].现代地质,1996,10(2):159-168.
    [6]
    朱光,王勇生,牛漫兰,等.郯庐断裂带的同造山运动[J].地学前缘,2004,11(3):169-182.
    [7]
    程捷,万天丰.郯庐断裂带在新生代的演化[J].地质科技情报,1996,15(3):36-43.
    [8]
    乔秀夫,张安棣.华北块体、胶辽朝块体与郯庐断裂[J].中国地质,2002,29(4):337-345.
    [9]
    吴根耀,马力,梁兴,等.从郯庐断裂带两侧的"盆""山"耦合演化看前白垩纪"郯庐断裂带"的性质[J].地质通报,2008,27(3):308-325.
    [10]
    吴根耀,梁兴,陈焕疆.试论郯城—庐江断裂带的形成、演化及其性质[J].地质科学,2007,42(1):160-175.
    [11]
    徐嘉炜,崔可锐,朱光,等.中国东部郯—庐断裂系统平移研究的若干进展[J].合肥工业大学学报,1984,1(2):28-37.
    [12]
    万天丰.中国中、新生代板内变形与构造应力场[J].地质力学学报,1996,2(3):13.
    [13]
    张岳桥,董树文.郯庐断裂带中生代构造演化史:进展与新认识[J].地质通报,2008,27(9):1371-1390.
    [14]
    朱光,刘国生,牛漫兰,等.郯庐断裂带的平移运动与成因[J].地质通报,2003,22(3):200-207.
    [15]
    徐嘉炜,朱光.中国东部郯庐断裂带构造模式讨论[J].华北地质矿产杂志,1995,10(2):121-134.
    [16]
    肖文交,周烑秀,杨振宇,等.大别—郯庐—苏鲁造山带复合旋转拼贴作用[J].地球科学进展,2000,15(2):147-153.
    [17]
    Gilder S A,Leloup P H.Tectonic evolution of the Tancheng-Lujiang (Tan-Lu) fault via middle Triassic to Early Cenozoic paleomagnetic data[J]. Journal of Geophysical Research,1999,104(7):15365-15390.
    [18]
    Yin A,Nie S Y.An indendation model for the North and South China collision and the development of the Tan-Lu and Honam fault system, eastern Asia[J].Tectonics,1993,12(4):801-803.
    [19]
    Chang E Z. Collision orogene between north and south China and its eastern extension in the Korean Peninsula[J]. Journal of Southeast Asian Earth Science,1996,13(3):267-277.
    [20]
    宗国洪.济阳坳陷构造演化及其大地构造意义[J].高校地质学报,1999,5(3):275-282.
    [21]
    汤良杰,陈绪云,周心怀,等.渤海海域郯庐断裂带构造解析[J].西南石油大学学报:自然科学版,2011,33(1):170-176.
    [22]
    王亮,牛成民,杨波,等.莱州湾凹陷沙三段含油气系统与有利勘探方向[J].断块油气田,2011,18(5):545-548.
    [23]
    牛成民.渤海南部海域莱州湾凹陷构造演化与油气成藏[J].石油与天然气地质,2012,33(3):424-431.
    [24]
    杨波,曾选萍,王改卫,等.莱州湾凹陷油气成藏主控因素分析[J].重庆科技学院学报:自然科学版,2011,13(1):6-9.
    [25]
    彭文绪,辛仁臣,孙和风,等.渤海海域莱州湾凹陷的形成和演化[J].石油学报,2009,30(5):654-660.
    [26]
    Yu Yixin,Zhou Xinhuai,Tang Liangjie,et al.Salt structures in the Laizhouwan depression, offshore Bohai Bay basin, eastern China: New insights from 3D seismic data[J].Marine and Petroleum Geology,2009, 26(8):1600-1607.
    [27]
    余一欣,周心怀,徐长贵,等.渤海海域新生代断裂发育特征及形成机制[J].石油与天然气地质,2011,32(2):273-279.
    [28]
    江涛,邱玉超,邓校国,等.狭长走滑断陷盆地构造对沉积—成藏的控制作用:以伊通盆地为例[J].石油实验地质,2012,34(3):267-271.
    [29]
    王永利,武强,王应斌.莱州湾凹陷西走滑带构造演化特征及对油气成藏的影响[J].石油地质与工程,2010,24(2):5-8.
    [30]
    邓运华.郯庐断裂带新构造运动对渤海东部油气聚集的控制作用[J].中国海上油气地质,2001,15(5):2-6.
    [31]
    马庆佑,沙旭光,李玉兰,等.塔中顺托果勒区块走滑断裂特征及控油作用[J].石油实验地质,2012,34(2):120-124.
    • 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 (1482) PDF downloads(1077) 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