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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2017  >  39(3): 409-416
Xu Nan, Xu Xi, Zhou Bo, Mei Fuding, Gao Shunli, Wang Xingjian. Physical simulation of Cenozoic tectonic deformation in the Lower Yangtze region and its main controlling factors[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2017, 39(3): 409-416. doi: 10.11781/sysydz201703409
Citation: Xu Nan, Xu Xi, Zhou Bo, Mei Fuding, Gao Shunli, Wang Xingjian. Physical simulation of Cenozoic tectonic deformation in the Lower Yangtze region and its main controlling factors[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2017, 39(3): 409-416. doi: 10.11781/sysydz201703409
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Physical simulation of Cenozoic tectonic deformation in the Lower Yangtze region and its main controlling factors

doi: 10.11781/sysydz201703409
  • 1.

    China University of Geosciences, Wuhan, Hubei 430074, China

  • 2. China Aero Geophysical survey and Remote Sensing Center for Land and Resources, Beijing 100083, China

  • 3. School of Ocean and Earth Science, Tongji University, Shanghai 200092, China

  • 4. Shanghai Branch of CNOOC China Ltd, Shanghai 200030, China

  • 5. State Key Laboratory of Oil and Gas Reservoir Geology and Exploration, Chengdu University of Technology, Chengdu, Sichuan 610059, China

  • Received Date: 2016-12-12
  • Rev Recd Date: 2017-03-17
  • Publish Date: 2017-05-28
    Abstract
  • The Cenozoic extensional tectonic deformation is an important window for the study of Cenozoic tectonic dynamics in East China. We evaluated four main controlling factors and designed seven sets of physical simulations to study the deformation mechanism of the Cenozoic structure in the Lower Yangtze region. The deformation process of the Lower Yangtze region during Cenozoic was simulated with different controlling factors. Stress angle and boundary position are the main factors controlling tectonic deformation. In the paralleled-experiments, the tectonic deformation of the Tan-Lu fault and the Lower Yangtze region and its surrounding blocks showed significant variations in boundary compression. In the paralleled-experiments of block thickness, deformation and displacement were similar, but there are significant differences in uplift characteristics and extrusion effects between east and west boundaries. With smaller angle between stress and model boundary, the Tan-Lu fault presented obvious dextral movement. In the simulation with optimal controlling factors, the extensional tectonics of the Lower Yangtze block and the dextral movement of the Tan-Lu fault formed a tectonic system with dextral strike-slip and lateral extension.

     

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    • References(19)
  • [1]
    Liu Mian,Cui Xiaojun,Liu Futian.Cenozoic rifting and volcanism in eastern China:A mantle dynamic link to the Indo-Asian collision[J].Tectonophysics,2004,393(1/4):29-42.
    [2]
    Huang Jinli,Zhao Dapeng.High-resolution mantle tomography of China and surrounding regions[J].Journal of Geophysical Research:Solid Earth,2006,111(B9):B09305.
    [3]
    Li Qiang,You Xinzhao,Yang Shaomin,et al.A precise velocity field of tectonic deformation in China as inferred from intensive GPS observations[J].Science China Earth Sciences,2012,55(5):695-698.
    [4]
    徐曦,高顺莉,王兴建,等.下扬子区新生代伸展构造变形及其区域构造意义[J].地球科学(中国地质大学学报),2015,40(12):1968-1986. Xu Xi,Gao Shunli,Wang Xingjian,et al.Cenozoic deformation of extensional tectonics in the Lower Yangtze region and its tectonic significance[J].Earth science (Journal of China University of Geosciences),2015,40(12):1968-1986.
    [5]
    徐曦,高顺莉.下扬子区新生代断陷盆地的构造与形成[J].地学前缘,2015,22(6):148-166. Xu Xi,Gao Shunli.The structure and formation of the Cenozoic fault basin in the Lower Yangtze region[J].Earth Science Frontiers,2015,22(6):148-166.
    [6]
    Xu Yigang.Diachronous lithospheric thinning of the North China craton and formation of the Daxin'anling-Taihangshan gravity lineament[J].Lithos,2007,96(1/2):281-298.
    [7]
    Becker J J,Sandwell D T,Smith W H F,et al.Global bathymetry and elevation data at 30 arc seconds resolution:SRTM30_PLUS[J].Marine Geodesy,2009,32(4):355-371.
    [8]
    Tapponnier P,Le Peltzer G,Le Dain A Y,et al.Propagating extrusion tectonics in Asia:New insights from simple experiments with plasticine[J].Geology,1982,10(12):611-616.
    [9]
    徐政语,林舸,刘池阳,等.从江汉叠合盆地构造形变特征看华南与华北陆块的拼贴过程[J].地质科学,2004,39(2):284-295. Xu Zhengyu,Lin Ge,Liu Chiyang,et al. A discussion on amalgamation course between the South China and North China blocks:Evidences from deformational characters in the Jianghan superimposed basin[J].Chinese Journal of Geology,2004,39(2):284-295.
    [10]
    Hou Guiting,Hari K R.Mesozoic-Cenozoic extension of the Bohai Sea:Contribution to the destruction of North China craton[J].Frontiers of Earth Science,2014,8(2):202-215.
    [11]
    周建勋,周建生.渤海湾盆地新生代构造变形机制:物理模拟和讨论[J].中国科学(D辑地球科学),2006,36(6):507-519. Zhou Jianxun,Zhou Jiansheng.Mechanisms of Cenozoic deforma-tion in the Bohai Basin,Northeast China:Physical modelling and discussions[J].Science in China(Series D Earth Science),2006,49(3):258-271.
    [12]
    周建勋,周天伟.南堡凹陷晚新生代X型断层形成机制及其对油气运聚的控制[J].大地构造与成矿学,2008,32(1):20-27. Zhou Tianwei,Zhou Jianxun.Formation mechanism of X-pattern normal faults during Late Cenozoic and their impact on hydrocarbon accumulation in the Nanpu Sag of Bohai Bay Basin[J].Geotectonica et Metallogenia,2008,32(1):20-27.
    [13]
    Li Shuguang,Xiao Yilin,Liou D,et al.Collision of the North China and Yangtze blocks and formation of coesite-bearing eclogites:Timing and processes[J].Chemical Geology,1993,109(1/4):89-111.
    [14]
    Li Jiahua,Zhang Yueqiao,Dong Shuwen,et al.Cretaceous tectonic evolution of South China:A preliminary synthesis[J].Earth-Science Reviews, 2014,134:98-136.
    [15]
    Zhang Jiaodong,Yang Xiaoyong,Sun W,et al.New data on the evolution of the Tan-Lu Fault Belt:Constraints from geological-geophysical surveys in the southern segment[J].International Geology Review,2012,54(13):1562-1578.
    [16]
    Chang K,Zhao Xixi.North and South China suturing in the east end:What happened in korean peninsula?[J].Gondwana Research,2012,22(2):493-506.
    [17]
    Mercier J L,Vergely P,Zhang Yueqiao,et al.Structural records of the Late Cretaceous-Cenozoic extension in eastern China and the kinematics of the southern Tan-Lu and Qinling fault zone (Anhui and Shaanxi provinces,PR China)[J].Tectonophysics,2013,582:50-75.
    [18]
    Huang Rong,Xu Yixian,Luo Yinhe,et al.Mantle transition zone structure beneath southeastern China and its implications for stagnant slab and water transportation in the mantle[J].Pure and Applied Geophysics,2014,171(9):2129-2136.
    [19]
    Hong T K,Choi H.Seismological constraints on the collision belt between the North and South China blocks in the Yellow Sea[J].Tectonophysics,2012,570-571:102-113.
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