留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

南海的盆地群与盆地动力学

李三忠 索艳慧 刘鑫 戴黎明 余珊 赵淑娟 马云 王霄飞 程世秀 安慧婷 薛友辰 熊莉娟 曹现志 许立青

李三忠, 索艳慧, 刘鑫, 戴黎明, 余珊, 赵淑娟, 马云, 王霄飞, 程世秀, 安慧婷, 薛友辰, 熊莉娟, 曹现志, 许立青. 南海的盆地群与盆地动力学[J]. 海洋地质与第四纪地质, 2012, 32(6): 55-78. doi: 10.3724/SP.J.1140.2012.06055
引用本文: 李三忠, 索艳慧, 刘鑫, 戴黎明, 余珊, 赵淑娟, 马云, 王霄飞, 程世秀, 安慧婷, 薛友辰, 熊莉娟, 曹现志, 许立青. 南海的盆地群与盆地动力学[J]. 海洋地质与第四纪地质, 2012, 32(6): 55-78. doi: 10.3724/SP.J.1140.2012.06055
LI Sanzhong, SUO Yanhui, LIU Xin, DAI Liming, YU Shan, ZHAO Shujuan, MA Yun, WANG Xiaofei, CHENG Shixiu, AN Huiting, XUE Youchen, XIONG Lijuan, CAO Xianzhi, XU Liqing. BASIN DYNAMICS AND BASIN GROUPS OF THE SOUTH CHINA SEA[J]. Marine Geology & Quaternary Geology, 2012, 32(6): 55-78. doi: 10.3724/SP.J.1140.2012.06055
Citation: LI Sanzhong, SUO Yanhui, LIU Xin, DAI Liming, YU Shan, ZHAO Shujuan, MA Yun, WANG Xiaofei, CHENG Shixiu, AN Huiting, XUE Youchen, XIONG Lijuan, CAO Xianzhi, XU Liqing. BASIN DYNAMICS AND BASIN GROUPS OF THE SOUTH CHINA SEA[J]. Marine Geology & Quaternary Geology, 2012, 32(6): 55-78. doi: 10.3724/SP.J.1140.2012.06055

南海的盆地群与盆地动力学


doi: 10.3724/SP.J.1140.2012.06055
详细信息
    作者简介:

    李三忠(1968-),博士,教授,博导,从事构造地质学及海洋地质学的教学和研究工作,E-mail:sanzhong@ouc.edu.cn

  • 基金项目:

    中国海洋大学中央高校财政专项资助成果

  • 中图分类号: P736.1

BASIN DYNAMICS AND BASIN GROUPS OF THE SOUTH CHINA SEA

More Information
  • 摘要: 南海发育有众多的新生代盆地,按发育位置,总体可分为陆架盆地、陆坡盆地和深海海盆,陆架、陆坡盆地成因上与大陆边缘的裂解、转换密切相关,可分为走滑拉分-伸展盆地群、挤出-断陷盆地群、伸展-俯冲挠曲型盆地群,这些盆地进一步发展可形成不同阶段的洋盆群,西南次海盆发育程度低,中央次海盆发育程度高,因而南海盆地群的盆地动力学不是单一的动力学机制下形成的,机制非常复杂多变。这些盆地新生代以来经历了神狐、南海、东沙等多期构造运动,形成了复杂的角度不整合分布,且这些角度不整合时空上存在一定迁移规律。伴随着盆地构造迁移演化,断裂、岩浆、沉积沉降中心、成藏、灾害等都表现出显著的跃迁规律。南海成因的动力学背景复杂,受多种因素影响,其中板块动力因素既有东侧太平洋板块俯冲、菲律宾海板块楔入的影响,又有西侧印度洋板块斜向俯冲、洋中脊俯冲,还可能有北侧青藏高原隆升、大陆块体挤出的影响;同时,深部底侵、拆沉、地幔柱、地幔水化过程等地幔动力学背景也不可忽视。最终提出南海海盆的开启模式可能为走滑拉分模式,与太平洋构造域演化关系更为密切。
  • [1] 李思田,黄家福,杨士恭,等.霍林河煤盆地晚中生代沉积构造史和聚煤特征[J].地质学报,1982(3):244-254,293

    -294.[LI Sitian, HUANG Jiafu, YANG Shigong, et al. Depositional and structural history of the late Mesozoic Huolinhe basin and its characteristics of coal accumulation[J].Acta Geologica Sinica,1982(3):244-254,293-294.]
    [2] 李三忠,许淑梅,单业华,等.渤海湾及邻区构造演化与盆地组合规律[J].海洋学报,2000,22(增刊):220-229.[LI Sanhzong, XU Shumei, SHAN Yehua, et al. The tectonic evolution and pattern of basin combination of the Bohai Gulf and its adjacent areas[J]. Acta Oceanologica Sinica,2000

    , 22(supplement):220-229.]
    [3] 戴春山.中国海域含油气盆地群和早期评价技术[M].北京:海洋出版社,2011.[DAI Chunshanl. Oil Gas Basin Group of China Seas and Early Resource Assessment Techniques[M].Beijing:China Ocean Press, 2011.]
    [4] 龚再升,李思田.北部大陆边缘盆地油气成藏动力学研究[M].北京:科学出版社,2004.[GONG Zaisheng, LI Sitian. Dynamic Research of Oil and Gas Accumulation in the Northern Marginal Basins of South China Sea[M].Beijing:Science Press,2004.]
    [5] 丁巍伟,王渝明,陈汉林,等.台西南盆地构造特征与演化[J].浙江大学学报:理学版,2004,31(2):216-220.

    [DING Weiwei, WANG Yuming, CHEN Hanlin, et al. Deformation characters and its tectonic evolution of the Southwest Taiwan Basin[J].Journal of Zhejiang University (Science Edition),2004,31(2):216-220.]
    [6] 钟建强,黄慈流,詹文欢,等.台西盆地新生代构造的演化[J].海洋与湖沼,1996(3):271-278.[ZHONG Jianqiang, HUANG Ciliu, ZHAN Wenhuan, et al. Cenozoic tectonic evolution in Taixi basin[J].Oceanologia et Limnologia Sinica,1996

    (3):271-278.]
    [7] 易海,钟广见,马金凤.台西南盆地新生代断裂特征与盆地演化[J].石油实验地质,2007,29(6):560-564.

    [YI Hai, ZHONG Guangjian, MA Jinfeng. Fracture characteristics and basin evolution of the Taixinan basin in Cenozoic[J].Petroleum Geology and Experiment,2007,29(6):560-564.]
    [8] 姚伯初.南海新生代的构造演化与沉积盆地[J].南海地质研究,1998(10):1-17.[YAO Bochu. The tectonic evolution and sedimentary basins of South China Sea in Cenozoic[J].Geological Research of South China Sea,1998

    (10):1-17.]
    [9] 塔尔尼.岛弧、海沟和弧后盆地[M].北京:海洋出版社,1984:135-144.[TA Er'ni. IslandIsland, Ocean Trench and Bank-arc Basic[M].Beijing:Chian Ocean Press,1984:135

    -144.]
    [10] 刘以宣,钟建强,詹文欢.南海及邻域新构造运动基本特征[J].海洋地质与第四纪地质,1994,14(4):1-13.

    [LIU Yixuan, ZHONG Jianqiang, ZHAN Wenhuan. Basic characteristics of neotectonism in South China Sea and its adjacent regions[J].Marine Geology and Quaternary Geology,1994,14(4):1-13.]
    [11] 丁巍伟,杨树峰,陈汉林,等.台湾岛以南海域新近纪的弧-陆碰撞造山作用[J].地质科学,2006,41(2):195-201.

    [DING Weiwei, YANG Shufeng, CHEN Hanlin. Arc-continent collision orogeny in offshore Taiwan during Neogene[J].Chinese Journal of Geology,2006,41(2):195-201.]
    [12] Pautot G, Rangin C, Briais A, et al. Spreading direction in the central South China Sea[J]. Nature, 1986, 321:150-154.
    [13] Suppe J. Kinematics of arc-continent collision, flipping of subduction and back-arc spreading near Taiwan[J].Mem Geol Soc China,1984,6:21-33.
    [14] Reed D L, Lundberg N, Liu C S, et al. Structure relations alone the margins of the offshore Taiwan accretionary wedge:implications for accretion and crustal kinematics[J]. Acta Geologica Taiwanica, 1992,30:105-122.
    [15] Huang C H, Xia K Y, Perter B. Structural evolution from Paleogene extention to Latest Miocene recent arc continent collision offshore Taiwan:comparison with on land geology[J].Journal of Asian Earth Sciences,2001,19:619-639.
    [16] Hall R, Sparkman W. Mantle structure and tectonic evolution of the region north and east of Australia[C]//Defining Australia:the Australian Plate as Part of Planet Earth. Geological Society of America Special Paper,2002.
    [17] Honza E, Fujioka K. Formation of arcs and backarc basins inferred from the tectonic evolution of Southeast Asia since the Late Cretaceous[J]. Tectonophysics, 2004, 384:2353.
    [18] Mitchell A H G, Leach T M. Epithermal Gold in the Philippines. Island Arc Metallogenesis, Geothermal Systems and Geology[M]. Academic Press London, San Diego, New York, Geology Series, 1991.
    [19] Fuller M, Haston R, Lin J L. Tertiary paleomagnetidm of regions around the South China Sea[J].Journal of Southeast Asian Earth Sciences,1991,6:161-184.
    [20] Lee T Y, Laever L A. Cenozoic plate reconstruction of southeast Asia[J].Tectonoohysica,1995,25:85-139.
    [21] Jolivet L, Huchon P, Rangin C. Tectonic setting of Western Pacific marginal basins[J]. Tectonphysics, 1989,160:23-47.
    [22] 黃奇瑜, 闫义, 赵泉鸿, 等. 台湾新生代层序:反映南海张裂、层序和古海洋变化机制[J]. 科学通报, 2012, 57:1842-1862.[HUANG Qiyu, YEN Yi, ZHAO Quanhong, et al. Cenozoic stratigraphy of Taiwan:Looking into rifting, stratigraphy and paleoceanography of South China Sea[J]. China Sci. Bull., 2012

    , 57, doi:10.1007/s11434-012-5349-y]
    [23] 谢锦龙,黄冲,向峰云.南海西部海域新生代构造古地理演化及其对油气勘探的意义[J].地质科学,2008,43(1):133-153.

    [XIE Jinlong, HUANG Chong, XIANG Fengyun. Evolution of Cenozoic tectonic-palaeogeography and its petroleum significance in the western South China Sea[J].Chinese Journal of Geology,2008,43(1):133-153.]
    [24] 洪汉净,李涛,虢顺民,等.莺-琼盆地构造复合及其与油气关系的研究[R].中海石油西部公司研究报告,1998.[HONG Hanzheng, LI Tao, GUO Shunmin, et al. Tectonic combination and research of oil and gas relation in Yinggegai-Qiongdongnan Basin[R].The Wesrtern Reseach Report of The CNOOC,1998.]
    [25] 茹克.南海北部边缘叠合式盆地的发育及其大地构造意义[J].石油与天然气地质,1988,9(1):22-31.

    [RU Ke. The development of superimposed on the northern margin of the South China Sea and its tectonic significance[J].Oil and Gas Geology,1988,9(1):22-31.]
    [26] 朱伟林,江文荣.北部湾盆地涠西南凹陷断裂与油气藏[J].石油学报,1998,19(3):6-10.

    [ZHU Weilin, JIANG Wenrong. Multistage rifting and petroleum systems in the north part of South China Sea[J].Acta Petrolei Sinica,1998,19(3):6-10.]
    [27] Leloup P H, Kienast J R. High-temperature metamorphism in a major strikeslip shear zone:the Ailao Shan-Red River, People's Republic of China[J].Earth and Planetary Science Letters, 1993,118:213-234.
    [28] 谢文彦,张一伟,孙珍,等.琼东南盆地断裂构造与成因机制[J].海洋地质与第四纪地质,2007,27(1):71-78.

    [XIE Wenyan, ZHANG Yiwei, SUN Zhen, et al. Characteristics and formation mechanism of faults in Qiongdongnan basin[J].Marine Geology and Quaternary Geology,2007,27(1):71-78.]
    [29] Allen C R, Han Yuan, K E Sich, et al. Study of the Quaternary activities of the red river fault (Ⅰ)-general survey of its contemporary activities and evidence of the active faulting[J].Journal of Seismological Research,1984(1):39-51.
    [30] 孙珍, 钟志洪, 周蒂.莺歌海盆地构造演化与强烈沉降机制的分析和模拟[J].地球科学——中国地质大学学报,2007,32(3):347-356.

    [SUN Zhen, ZHONG Zhihong, ZHOU Di. The analysis and analogue modeling of the tectonic evolution and strong subsidence in the Yinggehai Basin[J].Earth Science-Journal of China University of Geosciences, 2007,32(3):347-356.]
    [31] Metcalfe I. Gondwanaland origin, dispersion and accretion of South American[J].Earth Sciences, 1994,7:333-347.
    [32] Metcalfe I. Palaeozoic and Mesozoic geological evolution of the SE Asian region:multidisciplinary constraints and implications for biogeography[C]//Biogeography and Geological Evolution of SE Asia. Backhuys Publishers, Leiden, The Netherlands,1998:25-41.
    [33] 李献华, 周汉文, 丁式江, 等. 海南岛洋中脊型变质基性岩:古特提斯洋壳的残片?[J].科学通报, 2000, 45(1):84-89.

    [LI Xianhua, ZHOU Hanwen, DING Shijiang, et al.. Metamorphic Mid-oceanic mafic rocks in the Hainan Province:segments of Plaeo-Tethys oceanic crust?[J].Chinese Science Bulletin, 2000, 45(1):84-89.]
    [34] 许志琴,杨经绥,李海兵,等.印度-亚洲碰撞大地构造[J].地质学报,2011,85(1):1-33.

    [XU Zhiqin, YANF Jingsui, LI Haibing, et al. On the tectonics of the India-Asia collision[J].Acta Geologica Sinica, 2011,85(1):1-33.]
    [35] Taylor B, Hayes D E. Origin and history of the South China Sea Basin[C]//The Tectonic and Geologic Evolution of Southeast Asian Seas and Island Part 2. Geophysical Monograph Series, American Geophysical Union,1983,27:23-56.
    [36] Tan D N K, Lamy J M. Tectonic evolution of NW Sabah continental margin since the late Eocene[J]. Bulletin of the Geological Society of Malaysia,1990,27:241-260.
    [37] Hall R. Reconstructing Cenozoic SE Asia[M]//Tectonic Evolution of SE Asia. Geological Society of London Special Publication, 1996,106:153-184.
    [38] Briais A, Patriat P, Tapponnier P. Updated interpretation of magnetic anomalies and sea floor spreading stages in the South China Sea:implications for the Tertiary tectonics of Southeast Asia[J].Journal of Geophysical Research,1993,98:6299-6328.
    [39] Tapponnier P, Peltzer G, Le Dain, et al. Propagating extrusion tectonics in Asia:New insights from simple experiments with plasticine[J].Geology,1982,10:611-616.
    [40] Leloup P H, Lacassin R, Tapponier P, et al. The Ailao Shan-Red River shear zone (Yunnan, China), Tertiary transform boundary of Indochina[J].Tectonophysics,1995,251:3-84.
    [41] Wang E, Burchfiel B C. Interpretation of Cenozoic tectonics in the right-lateral accommodation zone between the Ailao Shan shear zone and the eastern Himalayan syntaxis[J]. International Geology Review, 1997,39:191-219.
    [42] Rangin C, Klein M, Roques D, et al. The Red River fault system in the Tonkin Gulf, Vietnam[J]. Tectonophysics,1995,243:209-222.
    [43] Ropues D, Rangin C, Huchon P. Geometry and sense of motion along the Vietnam margin:onshore/offshore Da Nang area[J]. Bulletin Dela, 1997b.
    [44] Lacassin R, Maluski H, Leloup P H, et al. Tertiary diachronic extrusion and deformation of western Indochina:Structural and Ar40/Ar39 evidence from NW Thailand[J].Journal of Geophysical Reseach,1997, 102:10013-10017.
    [45] Lacassin R, Replumaz A, Leloup P H. Hairpin river loops and slip-sense inversion on southeast Asian strike-slip fault[J].Geology,1998,26:703-706.
    [46] Satyabala S P. Subduction in the Indo-Burman region:is it still active?[J].Geophysical Reseach Letters,1998,25:3189-3192.
    [47] Guzman-Speziae M, N J F. Comment on subduction in the Indo-Burma region:is it still active? by S P Satyabala[J].Geophysical Reseach Letters,2000,27:1065-1066.
    [48] Rao N P, Kumar M P. Evidences for cessation of Indian plate subduction in the Burmeae arc region[J].Geophysical Reseach Letters,1999,26:3149-3152.
    [49] Krishna M R, Sanu T D. Seismotectonics and rates of active crustal deformation in the Burmese arc and adjacent regions[J].Journal of Geodynamics,2000,30:401-421.
    [50] Bertrand G, Rangin C, Maury R C, et al. The Singu basalts (Myanmar):new comptes for the amount of recent offset on the Sagaing Fault[J]. Computes de Rendus, 1998.
    [51] Curray J R, Moore D G, Laever L A, et al.Tectonics of the Andaman Sea and Burma. Geological and Geophysical Investigations of Continental Margins[M]//American Association of Petroleum Geologists Memoir,1979,29:189-198.
    [52] Mitchell A H G. Tectonic settings for emplacement of the Southeast Asian tin granites[J].Geological Society of Malaysia Bulletin,1977,9:123-140.
    [53] Hla Maung.Transcurrent movements in the Burma-Andaman Sea region[J].Geology, 1987,15(10):911-912.
    [54] Mitchell, A H G. Cretaceous-Cenozoic tectonic events in the western Myanmar (Burma) Assam region[J].Journal of the Geological Society,1973,150:1089-1102.
    [55] Andreason M W, Mudford B, Onge J E S. Geologic evolution and petroleum system of Thailand Andaman Sea Basins.[C]//Proceedings of the International Conference on Petroleum Systems of SE Asia and Australia. Indonesian Petroleum Association,1997:337-350.
    [56] Ni J F, Guzman-Speziale M, Bevis M, et al. Accretionary tectonics of Burma and the 3-dimensional geometry of the Burma subduction zone[J].Geology,1989,17:68-71.
    [57] Khin Zaw. Geological, petrological and geochemical characteristics of granitoid rocks in Burma:with special reference to the associated W-Sn mineralization and their tectonic setting[J].Journal of Southeast Asian Earth Sciences,1990,4:293-336.
    [58] Stephenson D, Marshall T R. The petrology and mineralogy of Mt Popa volcano and the nature of the Late Cenozoic Burma volcanic arc[J].Journal of the Geological Society of London,1984,141:747-762.
    [59] 龚再升,李思田,谢泰俊,等.南海北部大陆边缘盆地分析与油气聚集[M].北京:科学出版社,1997.[GONG Zaisheng, LI Sitian, XIE Taijun, et al. Continental Margin Basin Analysis and Hydrocarbon Aaccumulation of the Northern South China Sea[M].Beijing:Science Press,1997.]
    [60] Hsu S K, Sibuet J C. Is Taiwan the result of arc-continent or arc-arc collision?[J]. Earth and Planetary Science Letters, 1995, 136:315-324.
    [61] 夏斌,吕宝凤,吴国干,等.南海北部新生代盆地构造迁移及其对烃源岩的制约作用[J]. 天然气地球科学,2007,18(5):629-634.

    [XIA Bin, LV Baofeng, WU Guogan, et al.The Cenozoic tectonic transport and its control on the source rock in the northern South China Sea[J].Natural Gas Geoscience,2007,18(5):629-634.]
    [62] 蔡周荣,刘维亮,万志峰,等.南海北部新生代构造运动厘定及与油气成藏关系探讨[J].海洋通报,2010,29(2):161-165.

    [CAI Zhourong, LIU Weiliang, WAN Zhifeng,et al. Determination of Cenozoic tectonic movement in the northern South China Sea and the relationship between oil-gas reservoir and tectonic movement[J].Marine Science Bulletin,2010,29(2):161-165.]
    [63] 夏戡原,黄慈流,黄志明.南海及邻区中生代(晚三叠世-白垩纪)地层分布特征及含油气性对比[J].中国海上油气,2004,16(2):2-12.

    [XIA Kanyuan, HUANG Cliliu, HUANG Zhiming. Oil-bearing comparison and Mesozoic (Late Triassic-Creataceous) in the South China Sea and its neighbors[J].China Offshore Oil and Gas,2004,16(2):2-12.]
    [64] 吴世敏,周蒂,刘海龄.南沙地块构造格局及其演化特征[J].大地构造与成矿学,2004,28(1):23-28.

    [WU Shimin, ZHOU Di, LIU Hailing. Tectonic framework and evolutionary characteristics of Nansha Block, South China Sea[J].Geotectonica et Metallogenia,2004,28(1):23-28.]
    [65] Tayler B, Hays D E. Origin and history of South China Sea Basin[C]//The Tectonic and Geological Evolution of Southeast Asian Seas and Islands, American Geophysical Union, Geophysical monograph, Washington D C, 1983, 27:23256.
    [66] Holloway N H. The north Palawan block, Philippines:Its relation to the Asian mainland and its role in the evolution of the South China Sea[J]. Geological Society Malaysia Bulletin, 1982, 66(9):1355-1383.
    [67] Hamilton W. Tectonics of the Indonesian region[R]. U. S. Geol. Surv. Prof. Paper. 1979.
    [68] 夏戡源. 南沙群岛及其邻近海区地质地球物理与油气资源[M]. 北京:科学出版社, 1996.[XIA Kanyuan. Geology, Geophysics and Oil gas Gas Resources in Nansha Isle and its Neighboring Sea Areas[M]. Beijing:Science Press, 1996.]
    [69] Katili J A. Geology of Southeast Asia with particular reference to the South China Sea[J].Ministry of Mines and Energy,1981,6(11):1077-1091.
    [70] Hutchinson C S. Geological evolution of South-East Asia[C]//Oxford Monographs on Geology and Geophysics,Vol.13.Oxford, England:Clarendon Press, Oxford, 1989:368.
    [71] 孙珍, 赵中贤, 李家彪,等. 南沙地块内破裂不整合与碰撞不整合的构造分析[J]. 地球物理学报, 2011, 54(12):3196-3209

    [SUN Zhen, ZHAO Zhongxian, LI Jiabao, et al. Tectonic analysis of the breakup and collision unconformities in the Nansha[J]. Chinese Journal of Geophysics, 2011, 54(12):3196-3209].
    [72] 解习农,张成,任建业,等. 南海南北大陆边缘盆地构造演化差异性对油气成藏条件控制[J]. 地球物理学报,2011,54(12):3280-3291.

    [XIE Xinong, ZHANG Cheng, REN Jianye, et al.Effects of distinct tectonic evolutions on hydrocarbon accumulation in northern and southern continental marginal basins of South China Sea[J]. Chinese Journal of Geophysics, 2011,54(12):3280-3291.]
    [73] 孙珍,刘海龄.序:南海边缘海共轭陆缘构造-沉积过程研究的天然实验室[J].地球科学:地质大学学,2011,36(5):785-786.

    [SUN Zhen, LIU Hailing. Preface:Conjugate continental margins of the South China Sea-Natural laboratory of sedimentary proceses[J]. Earth Science-Journal of China University of Geosciences, 2011, 36(5):785-786.]
    [74]
    [75] Yu H S, Chow J. Cenozoic basins in northern Taiwan and tectonic implications for the development of the eastern Asian continental margin[J]. Tectonophysics, 1997, 131:133-144.
    [76] 徐发. 东海陆架盆地新生界结构特征及迁移规律[J]. 石油天然气学报, 2012, 34(6):1-7.

    [XU Fa. Characteriztics of Cenozoic structure and tectonic migration of the East China Sea Shelf Basin[J]. Journal of Oil and Gas Technology, 2012, 34(6):1-7.]
    [77] 索艳慧, 李三忠, 戴黎明, 等. 东海陆架盆地构造单元划分与特征[J]. 海洋地质与第四纪地质, 2010, 30(6):49-58.

    [SUO Yanhui, LI Sanzhong, DAI Liming, et al. Division and characteristics of tectonic units of the East China Sea Shelf Basin[J]. Marine Geology and Quaternary Geology, 2010, 30(6):49-58.]
    [78] 姚伯初.南海海盆新生代的构造演化史[J].海洋地质与第四纪地质,1996,16(2):1-13.

    [YAO Bochu. Tectonic evolution of the South China Sea[J].Marine Geology and Quaternary Geology,1996,16(2):1-13.]
    [79] Clift P, Lin J. Preferential mantle lithospheric extension under the South China margin[J]. Marine and Petroleum Geology, 2001, 18:929-945.
    [80] Clift P, Lee G H, Duc N A, et al. Seismic reflection evidence for a Dangerous Grounds miniplate:No extrusion origin for the South China Sea[J]. Tectonics, 2008, 27, TC3008, doi:10.1029/2007TC002216.
    [81] 汪品先. 追踪边缘海的生命史:"南海深部计划"的科学目标[J]. 科学通报,2012,57(20):1807-1826.

    [WANG Pinxian. Tracing the life history of a marginal Sea-On the "South China Sea Deep" Research Program[J]. China Sci. Bull, 2012, 57, doi:10.1007/s11434-012-5087-1].
    [82] Yeh Yiching, Sibuet J C, Hsu Shukun, et al. Tectonic evolution of the Northeastern South China Sea from seismic interpretation[J]. Journal of Geophysical Research, 2010, 115, B06103, doi:10. 1029/2009 JB006354.
    [83] 栾锡武,刘鸿,彭学超. 南海北部东沙古隆起的综合地球物理解释[J]. 地球物理学报,2011,54(12):3217-3232.

    [LUAN Xiwu, LIU Hong, PENG Xuechao. The geophysical interpretation of a Dongsha ancient uplift on the northern margin of South China Sea[J]. Chinese Journal of Geophysics, 2011,54(12):3217-3232.]
    [84] Hsu S K, Yeh Y C, Doo W B, et al. New bathymetry and magnetic lineations in the northernmost South China Sea and their tectonic implication[J]. Marine Geophysics Research, 2004, 25, 29-44, doi:10.1007/s11001-005-0731-7.
    [85] 李家彪,丁巍伟,高金耀, 等. 南海新生代海底扩张的构造演化模式:来自高分辨率地球物理数据的认识[J]. 地球物理学报,2011,54(12):3004-3015.

    [LI Jiabiao, DING Weiwei, GAO Jinyao, et al. Cenozoic evolution model of the sea-floor spreading in South China Sea:new constraints from high resolution geophysical data[J]. Chinese Journal of Geophysics, 2011,54(12):3004-3015.]
    [86] 孙珍,孙龙涛,周蒂,等.南海岩石圈破裂方式与扩张过程的三维物理模拟[J].地球科学-中国地质大学学报,2009,34(3):435-447.

    [SUN Zhen, SUN Haitao, ZHOU Di, et al. Discussion on the South China Sea evolution and lithospheric breakup through 3D analogue modeling[J].Earth Science-Journal of China University of Geosciences,2009,34(3):435-447.]
    [87] Huchon P, Hguyen T N H, Chamot-Rooke N. Propagation of continental breakup in the southwestern South China Sea[J]. Geological Society, 2001, 187(1):31-50.
    [88] 张洁,李家彪,李细兵,等. 渐进式扩张海盆亚丁湾与南海西南次海盆扩张演化特征的对比[J]. 地球物理学报,2011,54(12):3079-3088.

    [ZHANG Jie, LI Jiabiao, LI Xibing, et al. A comparison on tectonic evolution characteristics of ridge propagation between the Gulf of Aden and the Southwestern Sub-basin, South China Sea[J]. Chinese Journal of Geophysics, 2011,54(12):3079-3088.]
    [89] 李家彪, 丁巍伟, 吴自银, 等. 南海西南海盆的渐进式扩张[J]. 科学通报, 2012, 57:1896-1905.[LI Jiabiao, DING Weiwei, WU Ziyin, et al. The propagation of seafloor spreading in the southwestern subbasin, South China Sea[J]. China Sci Bull, 2012

    , 57, doi:10.1007/s11434-012-5329-2.]
    [90] 李三忠,郭晓玉,侯方辉,等. 洋中脊分段性及其拓展和叠接机制[J].海洋地质动态,2004,20(11):19-28.

    [LI Sanzhong., GUO Xiaoyu, HOU Fanghui, et al. Segmentation, propagation and overlapping at mid-oceanic ridge[J]. Marine Geology Letters, 2004,20(11):19-28.]
    [91] 姚伯初,万玲,吴能友.大南海地区新生代板块构造活动[J].中国地质,2004,31(2):113-122.

    [YAO Bochu, WAN Ling, WU Nengyou. Cenozoic plate tectonic activities in the great South China Sea area[J].Geology in China, 2004,31(2):113-122.]
    [92] 金庆焕,李唐根.南沙海域区域地质构造[J].海洋地质与第四纪地质,2000,20(1):1-8.

    [JIN Qinghuan, LI Tanggen. Regional geologic tectonics of the Nansha Sea area[J].Marine Geology and Quaternary Geology,2000,20(1):1-8.]
    [93] 栾锡武,张亮.南海构造演化模式:综合作用下的被动扩张[J].海洋地质与第四纪地质,2009,29(6):59-74.

    [LUAN Xiwu,ZHANG Liang. Tectonic evolution modes of South China Sea:passive spreading under complex actions[J].Marine Geology and Quaternary Geology,2009, 29(6):59-74.]
    [94] 李三忠,索艳慧,戴黎明,等.渤海湾盆地形成与华北克拉通破坏[J].地学前缘,2010,17(4):64-89.

    [LI Sanzhong, SUO Yanhui, DAI Liming, et al. Development of the Bohai Bay Basin and destruction of the North China Craton[J].Earth Science Frontiers,2010,17(4):64-89.]
    [95] Yin An. Cenozoic tectonic evolution of Asia:a preliminary synthesis[J]. Tectonophysics,2010,488:293-325.
    [96] Allen M B, Macdonald D I M, Zhao X, et al. Early Cenozoic two-phase extension and Late Cenozoic thermal subsidence and inversion of the Bohai Basin,North China[J].Marine Petroleum Geology,1997,14:951-972.
    [97] 许浚远,杨巍然,曾佐勋,等.南中国海成因:右行拉分作用与左行转换挤压作用交替[J].地学前缘,2004(3):193-206.[XU Junyuan, YANG Weiran, ZENG Zuoxun, et al. Genesis of South China Sea:Intervening of dextral pull-apart and sinistral transpression[J].Earth Science Frontiers, 2004

    (3):193-206.]
    [98] Windley B F, Maruyama S, Xiao W J. Delamination/thinning of sub-continental lithospheric mantle under eastern China:The role of water and multiple subduction[J].American Journal of Science, 2010,310(10):1250-1293.
    [99] 徐义刚, 魏静娴, 邱华宁, 等. 用火山岩制约南海的形成演化:初步认识与研究设想[J]. 科学通报, 2012, 57:1863-1878.[XU Yigang, WEI Jingxian, QIU Huaning, et al. Opening and evolution of the South China Sea constrained by studies on volcanic rocks:Preliminary results and aresearch design[J]. China Sci Bull, 2012

    , 57, doi:10.1007/s11434-011-4921-1]
    [100] Whittaker J M, M ller R D, Sdrolias M, et al. Sunda-Java trench kinematics,slab window formation and overriding plate deformation since the Cretaceous[J].Earth and Planetary Science Letters, 2007, 255(3-4):445-457.
    [101] 朱伟林,米立军.中国海域含油气盆地图集[M].北京:石油工业出版社,2010.[ZHU Weilin, MI Lijun. Oil and Gas Basin Atlas of China Sea[M].Beijing:Petroleum Industry Press,2010.]
    [102] Michael B W Fyhna, Lars O Boldreela, Lars H Nielsen. Geological development of the Central and South Vietnamese margin:Implications for the establishment of the South China Sea,Indochinese escape tectonics and Cenozoic volcanism[J].Tectonophysics,2009,478(3-4):184-214.
    [103] Dieter Franke, Udo Barckhausen, Ingo Heyde, et al. Seismic images of a collision zone offshore NW Sabah/Borneo[J].Marine and Petroleum Geology,2008,25:606-624.
    [104] Jashar Arfai, Dieter Franke, Christoph Gaedicke,et al. Geological evolution of the West Luzon Basin(South China Sea, Philippines)[J]. Marine Geophysics Reseach,2011,32:349-362.
    [105] 索艳慧,李三忠,刘鑫,等.中国东部NWW向活动断裂带构造特征:以张家口-蓬莱断裂带为例[J].岩石学报,2012.[SUO Yanhui, LI Sanzhong, LIU Xin, et al. Structural characteristics of NWW-trending active fault zones in East China:A case study of the Zhangjiakou-Penglai Fault Zone[J].Acta Petrologica Sinica,2012.]
    [106] 李显武,周新民.中国东南部晚中生代俯冲带探索[J].高校地质学报,1999,5(2):164-169.

    [LI Xianwu, ZHOU Xinmin. Exploration of subduction zone of Late Mesozoic in southeastern China[J].Geological Journal of China Universities,1999,5(2):164-169.]
    [107] Tapponnier P, Pelt zer G, Arm ijo P. On the mechanics of the collision between India and Asia[J].Geol Soc Lond Spec,Publ,1986,19:115-157.
    [108] Zhou D, Ru K, Chen H Z. Kinematics of Cenozoic extension on the South China Sea continental margin and its implications for the tectonic evolution of the region[J].Tectonophysics,1995,251:161-177.
    [109] Tian Z Y, Du Y L. Formation and evolution of the Yilan-Yitong graben[J]. Tectonophysics, 1987, 133(3/4):165-173.
    [110] Ren J Y, Tamaki K, Li S T,et al. Late Mesozoic and Cenozoic rifting and its dynamic setting in Eastern China and adiacent areas[J].Tectonophysics,2002,344(3/4):175-205.
    [111] 闫义,夏斌,林舸,等.南海北缘新生代盆地沉积与构造演化及地球动力学背景[J].海洋地质与第四纪地质,2005,25(2):53-61.

    [YAN Yi, XIA Bin, LIN Ge, et al. the sedimentary and tectonic evolution of the basins in the north margin of the South China Sea and geodynamic setting[J]. Marine Geology and Quaternary Geology, 2005,25(2):53-61.]
    [112] 陈文寄,李齐,汪一鹏.哀牢山-红河左旋走滑剪切带中新世抬升的时间序列[J].地质论评,1996,42(5):385-390.

    [CHEN Wenji, LI Qi, WANG Yipeng. Miocene diachronic uplift along the Ailao Mountains-Red River left-lateral strike-slip shear zone[J].Geological Review, 1996,42(5):385-390.]
    [113] Wang P. Proceeding of the Ocean Drilling Program Initial Reports[J].2000.
    [114] Zhao D P. Multi-scale seismic tomography and mantle dynamics[J].Gondwana Research,2009,15:297-323.
    [115] Jolivet L, Huchon P, Brun J P, et al. Arc deformation and marginal basin opening:Japan Sea as a case study[J].Journal of Geophysical Research,1991,96:4367-4384.
    [116] Jolivet L, Tamaki K. Neogene kinematics in the Japan Sea region and the volcanic activity of the northeast Japan arc[C]//Proceedings of the Ocean Drilling Program, Scientific Results, 1992:127-128,1311-1331.
    [117] Jolivet L, Tamaki K, Fournier M. Japan Sea, opening history and mechanism:a synthsis[J].Journal of Geophysical Research,1994,99:22237-22259.
    [118] Gilles Peltzer, Paul Tapponnier. Formation and evolution of strike-slip faults, rifts, and basins during the India-Asia collision:an experimental approach[J].Journal of Geophysical Research, 1988, 93(B12):15085-15117.
    [119] Le Pichona X, Angelier J. The hellenic arc and trench system:A key to the neotectonic evolution of the eastern mediterranean area[J].Tectonophysics,1979,60(1-2):1-42.
    [120] Northrup C J, Royden L H, Burchfiel B C. Motion of the Pacific plate relative to Eurasia and its potential relation to Cenozoic extension along the eastern margin of Eurasia[J]. Geology, 1995,23:719-722.
    [121] Yin A. Mode of Cenozoic east west extension in Tibet suggesting a common origin of rifts in Asia during the Indo-Asian collision[J].Journal of Geophysics Research, 2000,105:21745-21759.
    [122] Chough S K, Kwon S T, Ree J H, et al. Tectonic and sedimentary evolution of the Korean peninsula:a review and new view[J].Earth Sci.Rev.,2000,52:175-235.
    [123] Lewis J C, Byrne T B, Tang X M. A geologic test of the Kula Pacific Ridge capture mechanism for the formation of the West Philippine Basin[J].Geology Society of American Bulletin, 2002,114:656-664.
    [124] Leigh H Royden, B Clark Burchfiel, Robert D, van der Hilst. The Geological Evolution of the Tibetan Plateau[J].Science,2008,321(5892):1054-1058.
    [125] Maruyama S, Hasegawa A, Santosh M, et al. The dynamics of big mantle wedge, magma factory, and metamorphic-metasomatic factory in subduction zones[J].Gondwana Research,2009,16:414-430.
    [126] 臧绍先,宁杰远.菲律宾海板块与欧亚板块的相互作用及其对东亚构造运动的影响[J].地球物理学报,2002,45(2):188-197.

    [ZANG Shaoxian, NING Jieyuan. Interaction between Philippine (PH) Sea Plate and Eurasia (EU) Plate and its influence on the movement Eastern Asia[J].Chinese Journal of Geophysics, 2002,45(2):188-197.]
    [127] Taylor B, Hayes D E. The tectonic evolution of the South China Sea Basin[C]//The tectonic and Geologic evolution of Southeast Asian Seas and Islands. Geophysical Monograph Series, American Geophysical Union,1980,23:89-104.
    [128] 李家彪. 南海大陆边缘动力学:科学实验与研究进展[J]. 地球物理学报,2011,54(12):2993-3003.

    [LI Jiabiao. Dynamics of the continental margins of South China Sea:scientific experiments and research progresses[J]. Chinese Journal of Geophysics, 2011,54(12):2993-3003.]
  • [1] 高丹, 程日辉, 沈艳杰, 候世林, 付秋林, 王嘹亮.  北黄海盆地东部坳陷中生界次生孔隙的发育规律 . 海洋地质与第四纪地质, 2021, 41(5): 1-8. doi: 10.16562/j.cnki.0256-1492.2020121601
    [2] 曾志刚, 张玉祥, 陈祖兴, 李晓辉, 齐海燕, 王晓媛, 陈帅, 殷学博.  西太平洋弧后盆地的热液系统及其岩浆环境研究 . 海洋地质与第四纪地质, 2021, 41(5): 1-13. doi: 10.16562/j.cnki.0256-1492.2021070101
    [3] 程琳燕, 李磊, 高毅凡, 张威, 龚广传, 杨志鹏, 王潘.  琼东南盆地陵水凹陷海底周期阶坎底形的特征及成因 . 海洋地质与第四纪地质, 2021, 41(5): 1-8. doi: 10.16562/j.cnki.0256-1492.2021041902
    [4] 杜晓东, 彭光荣, 吴静, 蔡国富, 汪晓萌1, 索艳慧, 周洁.  珠江口盆地阳江东凹始新统的源汇过程:碎屑锆石定年及物源示踪 . 海洋地质与第四纪地质, 2021, 41(5): 1-14. doi: 10.16562/j.cnki.0256-1492.2021071301
    [5] 兰蕾, 李友川, 王一博.  南海南部海陆过渡相烃源岩的两类分布模式 . 海洋地质与第四纪地质, 2021, 41(5): 1-8. doi: 10.16562/j.cnki.0256-1492.2021011802
    [6] 李法坤, 戴黎明, 李三忠, 董昊, 刘泽, 占华旺, 王亮亮, 盛世强, 胡泽明, 王迪, 王宇.  构造-沉积耦合过程的数值模拟:以南海北部阳江凹陷为例 . 海洋地质与第四纪地质, 2021, 41(5): 1-12. doi: 10.16562/j.cnki.0256-1492.2021040601
    [7] 马晓理, 刘丽华, 徐行, 金光荣, 魏雪芹, 翟梦月.  南海南部浅表层柱状沉积物孔隙水地球化学特征对甲烷渗漏活动的指示 . 海洋地质与第四纪地质, 2021, 41(5): 1-14. doi: 10.16562/j.cnki.0256-1492.2020123101
    [8] 徐俊杰, 刘道涵, 陈松, 刘慧, 刘磊, 刘盼, 刘广宁.  北康盆地基底卷入断层特征及其对南海南部构造演化的启示 . 海洋地质与第四纪地质, 2021, 41(4): 116-128. doi: 10.16562/j.cnki.0256-1492.2020101701
    [9] 鲁银涛, 杨涛涛, 许小勇, 徐宁, 刘忻蕾, 闫春, 邵大力, 范国章, 吕福亮, 李东.  印度尼西亚库泰盆地下中新统混积序列特征研究 . 海洋地质与第四纪地质, 2021, 41(): 1-9. doi: 10.16562/j.cnki.0256-1492.2021051403
    [10] 范佳慧, 窦衍光, 赵京涛, 李军, 邹亮, 蔡峰, 陈晓辉, 李清.  东海外陆坡−冲绳海槽水体剖面地球化学特征与指示意义 . 海洋地质与第四纪地质, 2021, 41(): 1-15.
  • 加载中
计量
  • 文章访问数:  776
  • HTML全文浏览量:  67
  • PDF下载量:  14
  • 被引次数: 0
出版历程
  • 收稿日期:  2012-09-30
  • 修回日期:  2012-12-20

南海的盆地群与盆地动力学

doi: 10.3724/SP.J.1140.2012.06055
    作者简介:

    李三忠(1968-),博士,教授,博导,从事构造地质学及海洋地质学的教学和研究工作,E-mail:sanzhong@ouc.edu.cn

基金项目:

中国海洋大学中央高校财政专项资助成果

  • 中图分类号: P736.1

摘要: 南海发育有众多的新生代盆地,按发育位置,总体可分为陆架盆地、陆坡盆地和深海海盆,陆架、陆坡盆地成因上与大陆边缘的裂解、转换密切相关,可分为走滑拉分-伸展盆地群、挤出-断陷盆地群、伸展-俯冲挠曲型盆地群,这些盆地进一步发展可形成不同阶段的洋盆群,西南次海盆发育程度低,中央次海盆发育程度高,因而南海盆地群的盆地动力学不是单一的动力学机制下形成的,机制非常复杂多变。这些盆地新生代以来经历了神狐、南海、东沙等多期构造运动,形成了复杂的角度不整合分布,且这些角度不整合时空上存在一定迁移规律。伴随着盆地构造迁移演化,断裂、岩浆、沉积沉降中心、成藏、灾害等都表现出显著的跃迁规律。南海成因的动力学背景复杂,受多种因素影响,其中板块动力因素既有东侧太平洋板块俯冲、菲律宾海板块楔入的影响,又有西侧印度洋板块斜向俯冲、洋中脊俯冲,还可能有北侧青藏高原隆升、大陆块体挤出的影响;同时,深部底侵、拆沉、地幔柱、地幔水化过程等地幔动力学背景也不可忽视。最终提出南海海盆的开启模式可能为走滑拉分模式,与太平洋构造域演化关系更为密切。

English Abstract

参考文献 (128)

目录

    /

    返回文章
    返回