Advanced Search

Indexed by SCI、CA、РЖ、PA、CSA、ZR、etc .

Volume 20 Issue 1
Feb 2009
Turn off MathJax
Article Contents
Zhen Sun, Di Zhou, Shimin Wu, Zhihong Zhong, Keep Myra, Jianqun Jiang, Hao Fan. Patterns and Dynamics of Rifting on Passive Continental Margin from Shelf to Slope of the Northern South China Sea: Evidence from 3D Analogue Modeling. Journal of Earth Science, 2009, 20(1): 136-146. doi: 10.1007/s12583-009-0011-6
Citation: Zhen Sun, Di Zhou, Shimin Wu, Zhihong Zhong, Keep Myra, Jianqun Jiang, Hao Fan. Patterns and Dynamics of Rifting on Passive Continental Margin from Shelf to Slope of the Northern South China Sea: Evidence from 3D Analogue Modeling. Journal of Earth Science, 2009, 20(1): 136-146. doi: 10.1007/s12583-009-0011-6

Patterns and Dynamics of Rifting on Passive Continental Margin from Shelf to Slope of the Northern South China Sea: Evidence from 3D Analogue Modeling

doi: 10.1007/s12583-009-0011-6
Funds:

the National Basic Research Program of China 2009CB219401

the National Basic Research Program of China 2007CB41170405

the CAS Key Innovation Program KZCX3-SW-234-1

the National Natural Science Foundation of China 40876026

the National Natural Science Foundation of China 40576027

the Knowledge Innovation Program of the South China Sea Institute of Oceanology, CAS LYQY200704

the Open Fund of the Key Laboratory of Marine Geology and Environment, CAS 

More Information
  • Corresponding author: Wu Shimin, smwu@scsio.ac.cn
  • Received Date: 28 Oct 2008
  • Accepted Date: 01 Dec 2008
  • Affected by thermal perturbation due to mantle uprising, the rheological structure of the lithosphere could be modified, which could lead to different rifting patterns from shelf to slope in a passive continental margin. From the observed deformation style on the northern South China Sea and analogue modeling experiments, we find that the rift zone located on the shelf is characterized by half grabens or simple grabens controlled mainly by long faults with large vertical offset, supposed to be formed with normal lithosphere extension. On the slope, where the lithosphere is very hot due to mantle upwelling and heating, composite grabens composed of symmetric grabens developed. The boundary and inner faults are all short with small vertical offset. Between the zones with very hot and normal lithosphere, composite half grabens composed of half grabens or asymmetric grabens formed, whose boundary faults are long with large vertical offset, while the inner faults are relatively short. Along with the thickness decrease of the brittle upper crust due to high temperature, the deformation becomes more sensitive to the shape of a pre-existing weakness zone and shows orientation variation along strike. When there was a bend in the pre-existing weakness zone, and the basal plate was pulled by a clockwise rotating stress, the strongest deformation always occurs along the middle segment and at the transition area from the middle to the eastern segments, which contributes to a hotter lithosphere in the middle segment, where the Baiyun (白云) sag formed.

     

  • loading
  • Briais, A., Patriat, P., Tapponnier, P., 1993. Updated Interpretation of Magnetic Anomalies and Seafloor Spreading Stages in the South China Sea: Implications for the Tertiary Tectonics of Southeast Asia. Journal of Geophysical Research, 98(B4): 6299–6328 doi: 10.1029/92JB02280
    Brun, J. P., 1999. Narrow Rifts versus Wide Rifts: Inferences for the Mechanics of Rifting from Laboratory Experiments. Philosophical Transactions of the Royal Society of London (Series A), 357(1753): 695–712 doi: 10.1098/rsta.1999.0349
    Callot, J. P., Geoffroy, L., Brun, J. P., 2002. Development of Volcanic Passive Margins: Three-Dimensional Laboratory Models. Tectonics, 21(6): 1052. doi: 10.1029/2001TC-901019
    Callot, J. P., Grigne, C., Geoffroy, L., et al., 2001. Development of Volcanic Passive Margins: Two-Dimensional Laboratory Models. Tectonics, 20(1): 148–159 doi: 10.1029/2000TC900030
    Cande, S. C., Kent, D. V., 1995. Revised Calibration of the Geomagnetic Polarity Timescale for the Late Cretaceous and Cenozoic. Journal of Geophysical Research, 100(B4): 6093–6095 doi: 10.1029/94JB03098
    Carter, N. L., Tsenn, M. C., 1987. Flow Properties of Continental Lithosphere. Tectonophysics, 136(1–2): 27–63 http://www.onacademic.com/detail/journal_1000035579914810_71c5.html
    Chen, C., Shi, H., Xu, S., et al., 2003. The Condition of Oil and Gas Reservoir Formation in the East of Pearl River Mouth Basin. Science Press, Beijing (in Chinese)
    Clift, P., Lin, J., 2001. Preferential Mantle Lithospheric Extension under the South China Margin. Marine and Petroleum Geology, 18(8): 929–945 doi: 10.1016/S0264-8172(01)00037-X
    Clift, P., Lin, J., Barckhausen, U., 2002. Evidence of Low Flexural Rigidity and Lower Viscosity Lower Continental Crust during Continental Break-up in the South China Sea. Marine and Petroleum Geology, 19(8): 951–970 doi: 10.1016/S0264-8172(02)00108-3
    Clift, P., Sun, Z., 2006. The Sedimentary and Tectonic Evolution of the Yinggehai-Song Hong Basin and the Southern Hainan Margin, South China Sea: Implications for Tibetan Uplift and Monsoon Intensification. Journal of Geophysical Research, 111: B06405 doi: 10.1029/2005JB004048/full
    Corti, G., Bonini, M., Innocenti, F., et al., 2001. Centrifuge Models Simulating Magma Emplacement during Oblique Rifting. Journal of Geodynamics, 31(5): 557–576 doi: 10.1016/S0264-3707(01)00032-1
    Corti, G., Bonini, M., Conticelli, S., et al., 2003. Analogue Modelling of Continental Extension: A Review Focused on the Relations between the Patterns of Deformation and the Presence of Magma. Earth-Science Reviews, 63(3–4): 169–247 http://www.sciencedirect.com/science/article/pii/S0012825203000357
    Davis, M., Kusznir, N., 2004. Depth-Dependent Lithospheric Stretching at Rifted Continental Margins. In: Karner, G. D., Morris, J. D., Driscoll, N. W., et al., eds., Rheology and Deformation of the Lithosphere of Continental Margins. Columbia University Press, New York. 92–137
    Davy, P., Cobbold, P. R., 1991. Experiments on Shortening of a 4-Layer Model of the Continental Lithosphere. Tectonophysics, 188(1–2): 1–25 http://www.onacademic.com/detail/journal_1000035692967610_8018.html
    He, L. J., Xiong, L. P., Wang, J. Y., et al., 2001. Tectono-thermal Modeling of the Yinggehai Basin, South China Sea. Science in China (Series D), 44(1): 7–13 doi: 10.1007/BF02906880
    Huang, C. J., Zhou, D., Sun, Z., et al., 2005. Deep Crustal Structure of Baiyun Sag, Northern South China Sea as Revealed from Deep Seismic Reflection Profile. Chinese Science Bulletin, 50(11): 1131–1138 doi: 10.1360/04wd0207
    Kang, X. D., Zhao, W. C., Pan, Z. G., et al., 1994. Study on Architecture of Sequence Stratigraphic Framework of Beibuwan Basin, China. Earth Science—Journal of China University of Geosciences, 19(4): 493–502 (in Chinese with English Abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX199404013.htm
    Kirby, S. H., 1983. Rheology of the Lithosphere. Reviews of Geophysics, 21: 1458–1487 doi: 10.1029/RG021i006p01458
    Kirby, S. H., Kronenberg, A. K., 1987. Rheology of the Lithosphere: Selected Topics. Reviews of Geophysics, 25(6): 1219–1244 doi: 10.1029/RG025i006p01219
    Keep, M., 2003. Physical Modelling of Deformation in the Tasman Orogenic Zone. Tectonophysics, 375(1–4): 37–47 http://www.sciencedirect.com/science?_ob=ShoppingCartURL&_method=add&_eid=1-s2.0-S0040195103003329&originContentFamily=serial&_origin=article&_ts=1464729720&md5=0655195f88f293457354f6c9cd82fd97
    Li, P. L., 1994. Structural Features and Oil-and-Gas Accumulation in Pearl River Mouth Basin. Guangdong Geology, 9(4): 21–28 (in Chinese)
    Morley, C. K., 1994. Interaction of Deep and Shallow Processes in the Evolution of the Kenya Rift. Tectonophysics, 236(1–4): 81–91 http://www.sciencedirect.com/science?_ob=ShoppingCartURL&_method=add&_eid=1-s2.0-0040195194901708&originContentFamily=serial&_origin=article&_ts=1473082856&md5=50c38f753bd499ab45ef4a52c584f817
    Morley, C. K., 1999. Marked along-Strike Variations in Dip of Normal Faults-The Lokichar Fault, N. Kenya Rift: A Possible Cause for Metamorphic Core Complexes. Journal of Structural Geology, 21(5): 479–492 http://www.sciencedirect.com/science/article/pii/S0191814199000437
    Pang, X., 2004. Annual Report of Deep Water Fan System and Its Hydrocarbon Resources (in Chinese)
    Prodehl, C., Fuchs, K., Mechie, J., 1997. Seismic-Refraction Studies of the Afro-Arabian Rift System—A Brief Review. Tectonophysics, 278(1–4): 1–13 http://www.irsm.cas.cz/ext/ethiopia/materials/papers/virtual_library_geological_setting/Prodehl_etal_1997_refraction%20seismic%20Afrorift.pdf
    Pubellier, M., Cobbold, P. R., 1996. Analogue Models for the Transpressional Docking of Volcanic Arcs in the Western Pacific. Tectonophysics, 253(1–2): 33–52 http://www.onacademic.com/detail/journal_1000035330438910_4b55.html
    Qin, G. Q., 2000. Investigation to the Stratigraphy and Construction of the Comprehensive Geologic Columnar Section of Cenozoic Formation in Pearl River Mouth Basin. China Offshore Oil and Gas (Geology), 14(1): 21–28 (in Chinese with English Abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZHSD200001004.htm
    Ranalli, G., 1995. Rheology of the Earth. 2nd Edition. Chapman & Hall, London. 413
    Ranalli, G., Murphy, D. C., 1987. Rheological Stratification of the Lithosphere. Tectonophysics, 132(4): 281–295 doi: 10.1016/0040-1951(87)90348-9
    Roberts, A. M., Yielding, G., Kusznir, N. J., et al., 1993. Mesozoic Extension in the North Sea: Constraints from Flexural Backstripping, Forward Modelling and Fault Populations. In: Parker, J. R., ed., Petroleum Geology of Northwest Europe. Proceedings of the Fourth Conference. Geological Society of London, London. 1123–1136
    Ru, K., 1988. The Development of Superimposed Basin on the Northern Margin of the South China Sea and Its Tectonic Significance. Oil & Gas Geology, 9(1): 22–31 (in Chinese with English Abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYYT198801002.htm
    Shi, X. B., Qiu, X. L., Xia, K. Y., et al., 2003. Characteristics of Surface Heat Flow in the South China Sea. Journal of Asian Earth Sciences, 22(3): 265–277 doi: 10.1016/S1367-9120(03)00059-2
    Sun, Z., Pang, X., Zhong, Z. H., et al., 2005. Dynamics of Tertiary Tectonic Evolution of the Baiyun Sag in the Pearl River Mouth Basin. Earth Science Frontiers, 12(4): 489–498 (in Chinese with English Abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY200504024.htm
    Sun, Z., Zhou, D., Zhong, Z. H., et al., 2006. Research on the Dynamics of the South China Sea Opening: Evidence from Analogue Modeling. Science in China (Series D), 49(10): 1053–1069 doi: 10.1007/s11430-006-1053-6
    Sun, Z., Zhou, D., Sun, L. T., et al., 2009. Dynamic Analysis on the Rifting Stage of the Pearl River Mouth Basin through Analogue Modeling. Acta Geologica Sinica (in Press)
    White, N., 1990. Does the Uniform Stretching Model Work in the North Sea? In: Blundell, D., Gibbs, A., eds., Tectonic Evolution of North Sea Rifts. Oxford University Press, Oxford, UK. 217–239
    Zhang, Q. M., Hao, F., 1997. Evolution and Hydrocarbon System in Ying-Qiong Basin. Science in China (Series D), 27(2): 149–154 (in Chinese) doi: 10.1007/BF02877623
    Zhang, Y. F., Sun, Z., Zhou, D., et al., 2008. Stretching Characteristics and Its Dynamic Significance of the Northern Continental Margin of South China Sea. Science in China (Series D), 51(3): 422–430 doi: 10.1007/s11430-008-0019-2
    Zhou, D., Ru, K., Chen, H. Z., 1995. Kinematics of Cenozoic Extension on the South China Sea Continental Margin and Its Implications for the Tectonic Evolution of the Region. Tectonophysics, 251(1–4): 161–177 doi: 10.1016/0040-1951(95)00018-6
  • 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

    Figures(9)  / Tables(2)

    Article Metrics

    Article views(524) PDF downloads(38) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return