Advanced Search
Volume 35 Issue 3
. 
Turn off MathJax
Article Contents
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2013  >  35(3): 255-262
Zhang Yuhang, Tang Liangjie, Yun Lu, Xie Daqing, Qiu Haijun, Jiang Huashan. Features and controlling factors of differential structural deformation of Kalashayi Fault in Bachu Uplift, Tarim Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2013, 35(3): 255-262. doi: 10.11781/sysydz201303255
Citation: Zhang Yuhang, Tang Liangjie, Yun Lu, Xie Daqing, Qiu Haijun, Jiang Huashan. Features and controlling factors of differential structural deformation of Kalashayi Fault in Bachu Uplift, Tarim Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2013, 35(3): 255-262. doi: 10.11781/sysydz201303255
shu

Features and controlling factors of differential structural deformation of Kalashayi Fault in Bachu Uplift, Tarim Basin

doi: 10.11781/sysydz201303255
  • 1.

    State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum, Beijing 102249, China

  • 2. Basin & Reservoir Research Center, China University of Petroleum, Beijing 102249, China

  • 3. SINOPEC Northwest Oilfield Company, Urumqi, Xinjiang 830011, China

  • 4. Oil and Gas Resources Strategic Research Center, Ministry of Land and Resources, Beijing 100034, China

  • Received Date: 2012-11-30
  • Rev Recd Date: 2013-03-20
  • Publish Date: 2013-05-28
    Abstract
  • Based on latest seismic interpretation data,the features of differential deformation of the Kalashayi Fault in the central Bachu Uplift were analyzed by means of fault-related fold theory and balanced section technique.The Kalashayi Fault is an active fault of multiple stages in the Bachu Uplift.It has suffered several stages of deformation,such as the early Caledonian,the episode Ⅰ of the middle Caledonian,the late Hercynian and the early Himalayan.On the plane,two faults of different scales converge like scissors from SW to NE.In profile,the Kalashayi Fault is composed of ramp-flat blind thrust fault which slips in Cambrian and high-angle basement-involved thrust fault.Gypsum-salt rocks control the multi-level deformation features of the Kalashayi Fault.The difference of pre-structure in basement leads to the segmental deformation features.Regional stress field transition results in the poly-phase deformation features.

     

    • FullText(HTML)
  • loading
    • References(21)
  • [1]
    汤良杰,黄太柱,金文正,等.叠合盆地差异构造变形与油气聚集[J].地学前缘,2009,16(4):13-22.
    [2]
    贾承造,魏国齐.塔里木盆地构造特征与含油气性[J].科学通报,2002,47(增刊):1-8.
    [3]
    何文渊,李江海,钱祥麟,等.塔里木盆地巴楚断隆中新生代的构造演化[J].北京大学学报:自然科学版,2000,36(4):539-546.
    [4]
    林畅松,杨海军,刘景彦,等.塔里木盆地古生代中央隆起带古构造地貌及其对沉积相发育分布的制约[J].中国科学:D辑:地球科学,2009,39(3):306-316.
    [5]
    顾忆,邵志兵,赵明,等.塔里木盆地巴楚隆起油气保存条件与勘探方向[J].石油实验地质,2011,33(1):50-55.
    [6]
    吴礼明,丁文龙,赵松,等.塔里木盆地巴楚—麦盖提地区古构造研究[J].断块油气田,2012,19(1):6-11.
    [7]
    杨明慧,金之钧,吕修祥,等.塔里木盆地基底卷入扭压构造与巴楚隆起的形成[J].地质学报,2007,81(2):158-165.
    [8]
    朱德丰,刘和甫,吴根耀.塔里木盆地西部吐木休克断裂带的主要特征和构造演化[J].地质科学,2008,43(2):209-227.
    [9]
    王宏语,樊太亮,魏福军,等.塔里木盆地巴楚中部地区寒武系盐下构造发育特征[J].石油与天然气地质,2004,25(5):554-557.
    [10]
    张洪安,吴根耀,李曰俊,等.塔里木盆地西部巴楚断隆南界断裂带的主要特征和构造演化[J].地质通报,2011,30(10):1547-1556.
    [11]
    任建业,张俊霞,杨怀忠,等.塔里木盆地中央隆起带断裂系统分析[J].岩石学报,2011,27(1):219-230.
    [12]
    汤良杰,贾承造,皮学军,等.库车前陆褶皱带盐相关构造样式[J].中国科学:D辑:地球科学,2003,33(1):38-46.
    [13]
    Konstantinovskaya E,Malavieille J.Thrust wedges with décollement levels and syntectonic erosion:A view from analog models[J].Tectonophysics,2011,502(1):336-350.
    [14]
    Fagereng A.Wedge geometry,mechanical strength,and interseismic coupling of the Hikurangi subduction thrust,New Zea-land[J].Tectonophysics,2011,507(1/2):26-30.
    [15]
    Mitra S.Fold-accommodation faults[J].AAPG Bulletin,2002,86(4):271-693.
    [16]
    Higgins S,Davies R J,Clarke B.Antithetic fault Linkages in a deep water fold and thrust belt[J].Journal of Structural Geo-logy,2007,29(12):1900-1914.
    [17]
    Kostenko O V,Naruk S J,Hack W,et al.Structural evaluation of column-height controls at a toe-thrust discovery,deep-water Niger Delta[J].AAPG Bulletin,2008,92(12):1615-1638.
    [18]
    Reiter K,Kukowski N,Ratschbacher L.The interaction of two indenters in analogue experiments and implications for curved fold-and-thrust belt [J].Earth and Planetary Science Letters,2011,302(1/2):132-146.
    [19]
    李乐,侯贵廷,潘文庆,等.塔里木盆地巴楚地区二叠纪以来构造应力场解析[J].地质力学学报,2011,17(3):262-273.
    [20]
    陈咪咪,田伟,张自力,等.塔里木盆地二叠纪基性—中性—酸性岩浆岩的年代学及其地质意义[J].岩石学报,2010,26(2):559-572.
    [21]
    孟庆强,朱东亚,谢启来,等.塔中和巴楚地区深部流体活动控制因素及有利区预测[J].石油实验地质,2011,33(6):597-606.
    • 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 (1361) PDF downloads(677) 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