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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2014  >  36(3): 275-284
Yang Yong, Tang Liangjie, Jiang Huashan, Chen Gang, Xie Daqing, Li Meng, Cao Zicheng. Characteristics and deformation mechanism of staging differential fault activities in Bachu Uplift, Tarim Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2014, 36(3): 275-284. doi: 10.11781/sysydz201403275
Citation: Yang Yong, Tang Liangjie, Jiang Huashan, Chen Gang, Xie Daqing, Li Meng, Cao Zicheng. Characteristics and deformation mechanism of staging differential fault activities in Bachu Uplift, Tarim Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2014, 36(3): 275-284. doi: 10.11781/sysydz201403275
shu

Characteristics and deformation mechanism of staging differential fault activities in Bachu Uplift, Tarim Basin

doi: 10.11781/sysydz201403275
  • 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

  • Received Date: 2013-12-31
  • Rev Recd Date: 2014-04-20
  • Publish Date: 2014-05-28
    Abstract
  • Based on the interpretation and analysis of the typical seismic profiles, we determined the activity phases of the faults in the Bachu uplift by calculating the amounts and rates of shortening of regional geological sections, and discussed the characteristics and deformation mechanism of staging differential activity. Fault activities took place mainly during the middle Caledonian, early Hercynian, late Hercynian, early Himalayan, middle Himalayan and late Himalayan. They were controlled by regional tectonic setting, pre-existing basement faults, regional detachment layer and some other factors. Compressive stress which generated by the closure of oceanic basin and the collision of plates was the dynamic source of the fault activities. The pre-existing basement faults controlled the position and orientation of the later stage faults. The regional detachment layer controlled fault development and distribution horizons.

     

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    • References(22)
  • [1]
    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. He Wenyuan,Li Jianghai,Qian Xianglin,et al.The Meso-Cenozoic evolution of Bachu fault-uplift in Tarim Basin[J].Acta Scientiarum Naturalium Universitatis Pekinensis,2000,36(4):539-546.
    [2]
    丁文龙,林畅松,漆立新,等.塔里木盆地巴楚隆起构造格架及形成演化[J].地学前缘,2008,15(2):242-252. Ding Wenlong,Lin Changsong,Qi Lixin,et al.Structural framework and evolution of Bachu uplift in Tarim basin[J].Earth Science Frontiers,2008,15(2):242-252.
    [3]
    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. Gu Yi,Shao Zhibing,Zhao Ming,et al.Hydrocarbon preservation and exploration in Bachu Uplift of Tarim Basin[J].Petroleum Geology & Experiment,2011,33(1):50-55.
    [4]
    肖安成,杨树锋,李曰俊,等.塔里木盆地巴楚-柯坪地区新生代断裂系统[J].石油与天然气地质,2005,26(1):78-85. Xiao Ancheng,Yang Shufeng,Li Yuejun,et al.A studying of Cenozoic fracture systems in Bachu-Kalpin area,Tarim Basin[J].Oil & Gas Geology,2005,26(1):78-85.
    [5]
    肖安成,杨树锋,李曰俊,等.塔里木盆地巴楚隆起断裂系统主要形成时代的新认识[J].地质科学,2005,40(2):291-302. Xiao Ancheng,Yang Shufeng,Li Yuejun,et al.Main period for creation of fracture system in the Bachu Uplift,Tarim Basin[J].Chinese Journal of Geology,2005,40(2):291-302.
    [6]
    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. Ren Jianye,Zang Junxia,Yang Huaizhong,et al.Analysis of fault systems in the Central uplift Tarim Basin[J].Acta Petrologica Sinica,2011,27(1):219-230.
    [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):158-163. Yang Minghui,Jin Zhijun,Lü xiuxiang,et al.Basement-involved transpressional structure and the formation of the Bachu Uplift,Tarim Basin,Northwestern China[J].Acta Geologica Sinica,2007,81(2):158-163.
    [8]
    赵岩,李勇,吴根耀,等.塔里木盆地西部罗斯塔格地区断裂特征和活动时代[J].石油与天然气地质,2010,31(6):795-801. Zhao Yan,Li Yong,Wu Genyao,et al.Characteristics and timing of faults in Luositage area,the western Tarim Basin[J].Oil & Gas Geology,2010,31(6):795-801.
    [9]
    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. Zhang Hongan,Wu Genyao,Li Yuejun,et al.Main features and structural evolution of southern boundary fractural zone of the Bachu fault-rise in western Tarim Basin[J].Geological Bulletin of China,2011,30(10):1547-1556.
    [10]
    姚文倩,汤良杰,谢大庆,等.塔里木盆地色力布亚断裂带变形特征和演化史[J].石油与天然气地质,2013,34(4):522-527. Yao Wenqian,Tang Liangjie,Xie Daqing,et al.Deformation and tectonic evolution of the Selibuya fault zone in Tarim Basin[J].Oil & Gas Geology,2013,34(4):522-527.
    [11]
    杨海军,李曰俊,冯晓军,等.塔里木盆地玛扎塔格构造带断裂构造分析[J].地质科学,2007,42(3):506-517. Yang Haijun,Li Yuejun,Feng Xiaojun,et al.Analysis on thrustings of the Mazhatage structural belt in the Tarim Basin[J].Chinese Journal of Geology,2007,42(3):506-517.
    [12]
    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. Zhu Defeng,Liu Hefu,Wu Genyao.Main characteristics and structural evolution of the Tumxuk fault zone in the western Tarim Basin[J].Chinese Journal of Geology,2008,43(2):209-227.
    [13]
    孟庆龙,李曰俊,师骏,等.塔里木盆地西部色力布亚断裂和康西断裂的主要特征及活动时代[J].地质科学,2008,43(2):282-293. Meng Qinglong,Li Yuejun,Shi Jun,et al.Main characters and active ages of the Serikbuya and Kangxi faults in the western Tarim Basin[J].Chinese Journal of Geology,2008,43(2):282-293.
    [14]
    He G Y,He Z L,Zhang H G,et al.Paleozoic structural deformation of Bachu Uplift,Tarim Basin of Northwest China:Implications for plate drifting[J].Journal of Earth Science,2009,20(4):755-762.
    [15]
    杨庚,李本亮,杨海军,等.塔里木盆地巴楚隆起北缘阿恰基底卷入构造[J].地质论评,2012,58(1):32-40. Yang Geng,Li Liben,Yang Haijun,et al.Basement-involved wedge-shaped structure of Aqia fault in northern Magin of Bachu Uplift in Northwestern Tarim Basin,Northwest China[J].Geological Review,2012,58(1):32-40.
    [16]
    Tong D J,Zhang J X,Yang H Z,et al.Fault system,deformation style and development mechanism of the Bachu Uplift,Tarim Basin[J].Journal of Earth Science,2012,23(4):529-541.
    [17]
    刘亚雷,齐英敏,刘云翔,等.塔里木盆地阿恰构造带断裂构造分析[J].现代地质,2013,27(1):158-164. Liu Yalei,Qi Yingmin,Liu Yunxiang,et al.Tectonic analysis on Aqia Fault Belt in the Western Tarim Basin[J].Geoscience,2013,27(1):158-164.
    [18]
    张宇航,汤良杰,云露,等.塔里木盆地巴楚隆起卡拉沙依断层差异构造变形特征及其控制因素[J].石油实验地质,2013,35(3):255-262. Zhang Yuhang,Tang Liangjie,Yun Lu,et al.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.
    [19]
    Lin C S,Yang H J,Liu J Y.Paleostructural geomorphology of the Paleozoic central uplift belt and its constraint on the development of depositional facies in the Tarim Basin[J].Science in China :Series D,2009,52(6):823-834.
    [20]
    汤良杰.塔里木盆地演化和构造样式[M].北京:地质出版社,1996. Tang Liangjie.Evolution and Tectonic Patterns of Tarim Basin[M].Beijing:Geological Publishing House,1996.
    [21]
    贾承造.中国塔里木盆地构造特征与油气[M].北京:石油工业出版社,1997. Jia Chengzao.Structural characteristics and oil & gas in Tarim Basin[M].Beijing:Petroleum Industry Press,1997.
    [22]
    何登发,贾承造,李德生,等.塔里木多旋回叠合盆地的形成与演化[J].石油与天然气地质,2005,26(1):64-77. He Dengfa,Jia Chengzao,Li Desheng,et al.Formation and evolution of polycyclic superimposed Tarim Basin[J].Oil & Gas Geology,2005,26(1):64-77.
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