XUE Youchen, LI Sanzhong, LIU Xin, SUO Yanhui, DAI Liming, YU Shan, ZHAO Shujuan, WANG Pengcheng, XIONG Lijuan, AN Huiting, CHENG Shixiu, WANG Xiaofei, MA Yun. SEGMENTATION OF SUBDUCTION SYSTEM IN THE EASTERN SOUTH CHINA SEA AND DYNAMICS OF RELATED BASIN GROUPS[J]. Marine Geology & Quaternary Geology, 2012, 32(6): 129-147. DOI: 10.3724/SP.J.1140.2012.06129
Citation: XUE Youchen, LI Sanzhong, LIU Xin, SUO Yanhui, DAI Liming, YU Shan, ZHAO Shujuan, WANG Pengcheng, XIONG Lijuan, AN Huiting, CHENG Shixiu, WANG Xiaofei, MA Yun. SEGMENTATION OF SUBDUCTION SYSTEM IN THE EASTERN SOUTH CHINA SEA AND DYNAMICS OF RELATED BASIN GROUPS[J]. Marine Geology & Quaternary Geology, 2012, 32(6): 129-147. DOI: 10.3724/SP.J.1140.2012.06129
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SEGMENTATION OF SUBDUCTION SYSTEM IN THE EASTERN SOUTH CHINA SEA AND DYNAMICS OF RELATED BASIN GROUPS

  • 1 Key Lab of Submarine Geosciences and Exploration Techniques, Ministry of Education, Qingdao 266100, China;

  • 2 College of Marine Geoscience, Ocean University of China, Qingdao 266100, China

More Information
  • Received Date: September 29, 2012
  • Revised Date: December 19, 2012
    Graphical Abstract
    • Abstract
  • The east part of the South China Sea is located at the convergence zone between the Eurasian Plate and the Pacific Plate (the Philippine Sea Plate). To the east of the South China Sea, there are the Manila Subduction Zone, the Luzon Arc and the East Luzon Philippine Subduction Zone, consisting of a opposite-dipping trench-arc-basin system which is called subduction system in this paper. The system can be subdivided into three segments from north to south by the Babuyan Strike-slipping Fault and the Sibuyan Strike-slipping Fault respectively, based on the differences in geomorphology, earthquakes, volcanism, faulting, basins and geophysical characteristics. The north segment is affected by the collision of the Taiwan Orogen, and the NWW-directed indentation of the Philippine Sea Plate and the stopping of the Beikang Uplift to the west of the Taiwan Orogen, resulted in the extrusion of the continental blocks of northeastern South China Sea, and the formation of the Taixinan Basin and the Taixi Basin,which are a series of collision-wedge-extrusion related basins. The middle segment is controlled by "Slab Window" during the subduction of fossil mid-oceanic ridge of the South China Sea, the earthquakes, magmatism, geomorphology and stress fields are different from north to south, and the formation of the basin group is controlled by arc strike-slip faults. The south segment is dominated by west-dipping subduction of the Philippine Sea Plate. The intensive earthquakes and volcanism are near the Philippine Trench. However, the stopping of the Sunda Block and the Palawan Block to the west of the Manila trench and the adjustment of the Great Philippine Fault in the central Philippine islands result in curvature of the Manila Trench in plane and decrease in earthquakes and volcanism in the west of the segment. The basin group is located in the segment developed on the basement resulting from collisions of different block fragments. The adjustment and pull-apart faulting of strike-slip faults caused the present-day basin pattern and distribution. The subduction system in the east of the South China Sea is affected by the NNW-directed indentation in the north segment and west-directed subduction in the south segment of the Philippine Plate, while the tectonic evolution of the middle segment of the subduction system is dominated by the east-directed subduction of the Manila Trench.
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    • References (68)
  • [1]
    Taylor B, Hayes D E. Origin and history of the South China Sea Basin[C]//Tectonic and Geological Evolution of Southeast Asian Seas and Islands, Part2, Geophys Monogr. Ser. 27.Washington D C:AGU, 1983:1-22.
    [2]
    Schweller W J, Karig D E, Bachman S B. Original setting and emplacement history of the Zambales ophiolite, Luzon, Phillipines, from stratigraphic evidence[C]//Tectonic and Geological Evolution of Southeast Asian Seas and Islands, Part2, Geophys Monogr. Ser. 27. Washington DC:AGU, 1983:124-138.
    [3]
    周蒂,陈汉宗,吴世敏,等.南海的右行陆缘裂解成因[J].地质学报,2002, 76(2):180-190.

    [ZHOU Di, CHEN Hanzong, WU Shimin, et al. Open of the South China Sea by dextral splitting of the East Asian continental margin[J]. Acta Geologica Sinca,2002, 76(2):180-190.]
    [4]
    朱俊江,丘学林,詹文欢,等.南海东部海沟的震源机制及其构造意义[J].地震学报,2005,27(3):260-268.

    [ZHU Junjiang, QIU Xuelin, ZHAN Wenhuan, et al. Focal mechanism solutions and its tectonic significance in the trench of the eastern South China Sea[J]. Acta Seismologica Sinica, 2005, 27(3):260-268.]
    [5]
    臧绍先,陈奇志,黄金水.台湾南部-菲律宾地区的地震分布、应力状态及板块的相互作用[J].地震地质, 1994,16(1):29-37.

    [ZANG Shaoxian, CHEN Qizhi, HUANG Jinshui. Distribution of earthquakes, the stress state and plate interactions in the southern Taiwan-Philippines[J]. Seismology and Geology, 1994,16(1):29-37.]
    [6]
    Yang T F, Lee T, Chen C H, et al. A double island arc between Taiwan and Luzon:consequence of ridge subduction[J]. Tectonophysics, 1996, 258:85-101.
    [7]
    李刚,张丽莉, 孙鲁.中国大陆边缘构造活动与重磁特征研究[J].地球物理学进展,2011,26(3):858-875.

    [LI Gang, ZHANG Lili, SUN Lu.Research on the tectonic features and gravity-magnetic characteristics of continental margins in the South China Sea[J]. Progress in Geophysics,2011,26(3):858-875.]
    [8]
    Bautista B C, Bautista M P, Oike K, et al. A new insight on the geometry of subducting slabs in northern Luzon, Philippines[J]. Tectonophysics, 2001,339:279-310.
    [9]
    李家彪,金翔龙,阮爱国,等.马尼拉海沟增生楔中段的挤入构造[J].科学通报, 2004,49(10):1000-1008.

    [LI Jiabiao, JIN Xianglong, RUAN Aiguo, et al. Diapiric structure at the middle segment of the accretionary wedge in Manila Trench[J]. Chinese Science Bulletin, 2004, 49(10):1000-1008.]
    [10]
    尹延鸿.试探马尼拉海沟的成因[J].海洋地质与第四纪地质,1988, 8(2):38-45.

    [YIN Yanhong. The origin of the Manila Trench[J]. Marine Geology and Quaternary Geology, 1988, 8(2):38-45.]
    [11]
    Sibueta J C. How was Taiwan created[J]. Tectonophysics, 2004, 379:159-181.
    [12]
    刘再峰,詹文欢,张志强.台湾-吕宋双火山弧的构造意义[J].大地构造与成矿学, 2007,31(2):146-150.

    [LIU Zaifeng, ZHAN Wenhuan, ZHANG Zhiqiang. Tectonic implication of the double island arc between Taiwan, Luzon[J]. Geotectonica et Metallogenia, 2007,31(2):146-150.]
    [13]
    许鹤华,周蒂.台湾造山带和前陆盆地的岩石圈热流变结构的模拟研究[C]//庆祝中国力学学会成50周年暨中国力学学术大会200论文摘要集(下).2007.[XU Hehua, ZHOU Di. Lithospheric thermal-rheological structure of the Taiwan Orogenic Belt and foreland basin simulation[C]//To celebrate the 50th anniversary of the establishment of the Chinese Society of Theoretical and Applied Mechanics, Mechanics 200

    Academic Conference Abstract Book,Part 2.2007.]
    [14]
    李家彪.中国边缘海形成演化与资源效应[M]. 北京:海洋出版社,2005:361-363.[LI Jiabiao. Formation, Evolution and Resource Effects of the Marginal Seas of China[M]. Beijing:Ocean Press,2005:361

    -363.]
    [15]
    Pautot G, Rangin C. Subduction of the South China Sea axial ridge below Luzon (Philippines)[J]. Earth and Planetary Science Letters,1989,92:57-69.
    [16]
    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):1-14.

    [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):1-14.]
    [17]
    陈学波,李金森,王恩福,等.汕头-吕宋岛岩石圈速度结构域震源构造[J].地球物理学进展, 1996,11(1):29-41.

    [CHEN Xuebo, LI Jinsen, WANG Enfu, et al. The velocity structure and the focal structure of the lithosphere on Shantou-Luzon Island[J]. Progress in Geophysics, 1996,11(1):29-41.]
    [18]
    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.]
    [19]
    李常珍,李乃胜,林美华.菲律宾海的地势特征[J]. 海洋科学,2000, 24(6):47-51.

    [LIN Meizhen, LI Naisheng, LIN Meihua. Terrain features of the Philippine Sea[J]. Journal of Marine Science, 2000, 24(6):47-51.]
    [20]
    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, 384:23-53.
    [21]
    郑彦鹏,刘保华,吴金龙,等.台湾岛以东海域加瓜楔形带对冲绳海槽南段的构造控制[J].中国科学D辑:地球科学,2005,35(1):88-95.

    [ZHENG Yanpeng, LIU Baohua, WU Jinlong, et al. The topographical characteristics in the area off eastern Taiwan Island and their tectonic implication[J]. Science China D Earth Sciences, 2005,35(1):88-95.]
    [22]
    Hall R J R, Ali C D, Anderson C D, et al. Origin and motion history of the Philippine Sea Plate[J]. Tectonophysics,1995, 251:229-250.
    [23]
    瞿辰,周蕙兰,赵大鹏.使用纵波和横波走时层析成像研究菲律宾海板块西边缘带和南海地区的深部结构[J]. 地球物理学报, 2007, 50(6):1757-1768.

    [QU Chen, ZHOU Huilan, ZHAO Dabao. Deep structure beneath the west margin of Philippine Sea Plate and South China Sea from P and S wave travel time tomography[J]. Chinese Journal of Geophysics, 2007,50(6):1757-1768]
    [24]
    丁巍伟,程晓敢,陈汉林,等.台湾岛增生楔的构造单元划分及其变形特征[J].热带海洋学报, 2005, 24(5):53-59.

    [DING Weiwei, CHENG Xiaogan, CHEN Hanlin, et al. Geological characteristics and tectonic mechanism of Taiwan accretionary prism:evidences from a multi-channel seismic profile of a"973"survey[J]. Journal of Tropical Oceanography, 2005,24(5):53-59.]
    [25]
    林美华,李乃胜.琉球海沟构造地貌[J].青岛海洋大学学报,1998, 28(3):497-501.

    [LIN Meihua, LI Naisheng. Tectonic geomorphology of the Ryukyu Trench[J]. Journal of Ocean University of Qingdao, 1998,28(3):497-501.]
    [26]
    Lewis S D, Hayes D E. The tectonics of northward propagating subduction along East Luzon, Philippine island[C]//The Tectonic and Geologic Evolution of Southeast Asian Seas and Islands, Part 2. Am. Geophys. Union, Geophys. Monogr. 1983, 27:57-78.
    [27]
    Hamburger M W, Cardwell R K, Isacks B L. Seismotectonics of the northern Philippine island arc[C]//The Tectonic and Geologic Evolution of Southeast Asian Seas and Islands, Part 2. Am. Geophys. Union, Geophys. Monogr, 1983, 27:1-22.
    [28]
    Grindlay N R,Fox P J,Vogt P R. Morphology and tectonics of the mid-Atlantic ridge from sea Beam and magnetic data[J]. Journal of Geophyiscal Research, 1992, 97:6983-7010.
    [29]
    杨蜀颖,方念乔,杨胜雄,等.关于南海中央次海盆海山火山岩形成背景与构造约束的再认识[J]. 地球科学, 2011, 36(3):455-470.

    [YANG Shuying, FANG Nianqiao,YANG Shengxiong, et al. A further discussion on formation background and tectonic constraints of igneous rocks in central sub-basin of the South China Sea[J]. Earth Science-Journal of China University of Geosciences, 2011, 36(3):455-470.]
    [30]
    李家彪,金翔龙,高金耀. 南海东部海盆晚期扩张的构造地貌研究[J].中国科学, 2002,32(3):240-247.

    [LI Jiabiao, JIN Xianglong, GAO Jinyao. The study of tectonic geomorphology of the late spreading in the eastern subbasin of South China Sea[J].Science in China (Series D), 2002,32(3):240-247.]
    [31] 尚继宏.马尼拉海沟中北段俯冲带特征对比及区域构造动力学研究[D].2008.[SHANG Jihong. Tectonic dynamics research and subduction characteristics comparison between middle and northern part of manila subducting belt[D].2008.]
    [32]
    杨马陵,魏柏林.南海海域地震海啸潜在危险的探析[J].灾害学,2005,20(1):43-44.

    [YANG Maling,WEI Bailin. The potential seismic Tsunami Risk in South China Sea and it's surrounding region[J]. Journal of Catastrophology, 2005, 20(1):43-44.]
    [33]
    Aurelio M. Shear partitioning in the Philippines:constraints from Philippine Fault and global positioning system data[J]. Island Arc, 2000, 9:584-597.
    [34]
    Quebral R D. Tectonique du segment meridionale de la faille Philippine, Mindanao oriental, Philippines:passage dune zone de collision a une zone de decrochement[C]//These de doctordt de l'universite Pierre et Marie Curie (Paris VI). Paris. France,1994:250.
    [35]
    钟建强,黄慈流,詹文欢.台湾海峡台西盆地新生代构造事件的分析[J].台湾海峡, 1994, 13(4):324-329.

    [ZHONG Jianqiang, HUANG Ciliu, ZHAN Wenhuan. Analyses of Cenozoic tectonic events in the Taixi Basin, Taiwan Strait[J]. Journal of Oceanography in Taiwan Strait, 1994,13(4):324-329.]
    [36]
    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 & Experiment, 2007, 29(6):560-564.]
    [37]
    钟广见,吴能友,林珍,等.南海东北陆坡断裂特征及其对盆地演化的控制作用[J].中国地质, 2008,35(3):458-459.

    [ZHONG Guangjian, WU Nengyou, LIN Zhen,et al. Characteristics of faults on the northeastern continental slope of the South China Sea and their controls on basin evolution[J]. Geology in China, 2008, 35(3):458-459.]
    [38]
    Schnürle P H, Liu C S, Lin A T, et al. Structural controls on the formation of BSR over a diapiric anticline from a dense MCS survey offshore southwestern Taiwan[J]. Marine and Petroleum Geology, 2011, 28:1932-1942.
    [39]
    Bautista B C, Bautista M P, Oike K, et al. A new insight on the geometry of subducting slabs in northern Luzon, Philippines[J]. Tectonophysics, 2001, 339:279-310.
    [40]
    Arfai J, Franke D, Gaedicke C, et al. Geological evolution of the West Luzon Basin(South China Sea, Philippines)[J]. Marince Geophysic Research, 2011, 32:349-362.
    [41]
    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].中国物理学报, 2002,45(2):189-197.

    [ZANG Shaoxian, NING Jieyuan. Interaction between Philippine Sea Plate and Eurasia Plateand its influence on the movement of eastern Asia[J]. Chinese Journal of Geophysics,2002, 45(2):189-197.]
    [42]
    李三忠,郭晓玉,侯方辉,等.活动大陆边缘的板片窗构造[J].海洋地质动态, 2004,20(11):6-18.

    [LI Sanzhong, GUO Xiaoyu, HOU Fanghui, et al. Slab window in the active continental margin[J]. Marine Geology Letters, 2004, 20(11):6-18.]
    [43]
    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 Chunshan. Oil Gas Baisn Group of China Seas and Early Resource Assessment Techniques[M]. Beijing:Ocean press, 2011.]
    [44]
    金庆焕,高天钧,黄辉,等.台湾海域中、新生代地质构造及油气前景[M].福州:福建科学技术出版社,1993.[JIN Qinghuan, GAO Tianjun, HUANG Hui, et al. The Taiwan Seas Geological Structure in Mesozoic and Cenozoic and Oil Gas Prospects[M]. Fuzhou:Fujian Science and Technology Press, 1993.]
    [45]
    钟建强,黄慈流,詹文欢,等.台西盆地新生代构造的演化[J].海洋与湖泊,1996, 27(23):271-278.

    [ZHONG Jianqiang, HUANG Ciliu, ZHAN Wenhuan, et al. Cenozoic tectonic evolution in Taixi Basin[J]. Oceanologia et Limnologia Sinica, 1996, 27(23):271-278.]
    [46]
    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.]
    [47]
    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(1):161-177.
    [48]
    Teng L S. Tectonic evolution of late Cenozoic arc continent collision in Taiwan[J]. American Association of Petroleum Bulletin, 1990, 74(6):1004-1005.
    [49]
    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.
    [50]
    Hirtzel J, Chi W C, Reed D, et al. Destruction of Luzon forearc basin from subduction to Taiwan arc continent collision[J]. Tectonophysics, 2009, 479:43-51.
    [51]
    Karig D E, Sarewitz D R, Haeck G D. Role of strike-slip faulting in the evolution of allocthonous terranes in the Philippines[J]. Geology, 1986,14:852-855.
    [52]
    Arfai J, Franke D, Gaedicke C, et al. Geological evolution of the West Luzon Basin(South China Sea, Philippines)[J]. Marince Geophysic Research,2011,32:349-362.
    [53]
    Ludwig W J, Hayes D E, Ewing J I. The manila Trench and West Luzon trough I. Bathymetry and sediment distribution[J]. Deep Sea Research, 1967(14):533-544.
    [54]
    Hayes D E, Lewis S E. Structure and tectonics of the Manila Trench system, Western Luzon, Philippines[J]. Energy, 1985, 10(3/4):263-279
    [55]
    Dickinson W R. Forearc basins[C]//Tectonics of sedimentary basins. Blackwell Science, Cambridge, 1995:221-262.
    [57]
    Aurelio M A,Pena R E. Geology and Mineral Resources of the Philippines-Volume 1:Geology. Department of Environment and Natural Resources-Mines and Geosciences Bureau[M]. 2002:391.
    [58]
    Barrier B, Huchon P, Aurelio M. Philippine Fault:a key for Philippine kinematics[J]. Geology, 1991(1):32-35.
    [59]
    邓属予.台湾新生代大地构造[M].中国地质学会、中国地球物理学会联合出版社,2002:49-95.[DENG Shuyu. Taiwan tectonics in Cenozoic[M]. United Press of the and Chinese Geophysical Society, 2002:49

    -95.
    [60]
    Whittaker J M, Müller R D, Sdrolias M U,et al. Sunda-Java trench kinematics, slab window formation and overriding plate deformation since the Cretaceous[J]. Earth and Planetary Science Letters,2007,255:445-457.
    [61]
    Yumul Jr G P, Dimalanta C B, Maglambayan V B, et al. Mineralization Controls in Island Arc Settings:Insights from Philippine Metallic Deposits[J]. Gondwana Research, 2003, 6(4):767-776
    [62]
    Wang T K, Chen M K, Lee C S,et al.Seismic imagine of the transitional crustal arcoss the northeastern margin of the South China Sea[J]. Tectonophysics, 2006, 412:237-254.
    [63]
    Thorkelson D J. Subduction of diverging plates and the principles of slab window formation[J]. Tectonophysics, 1996, 255:47-63.
    [64]
    孙金龙,徐辉龙,曹敬贺.台湾-吕宋会聚带的地壳运动特征及其动力学机制[J].地球物理学报,2011,54(12):3016-3025.

    [SUN Jinlong, XU Huilong, CAO Jinghe.Crustal movement and its dynamic mechanism of the Taiwan-Luzon convergent zone[J].Chinese Journal of Geophysics, 2011,54(12):3016-3025.]
    [65]
    李春峰,周祖翼,李家彪,等.台湾岛南部海域的前碰撞构造地球物理特征[J].中国科学,2007,37(05):649-659.

    [LI Chun-feng, ZHOU Zuyi, LI Jiabiao,et al. Before collisional tectonic geophysical characteristics of the offshore southern Taiwan[J]. Science in China, 2007,37(5):649-659.]
    [66]
    刘海龄,孙岩,郭令智,等.2001.南沙微板块边界的动力学演化[J]. 海洋学报,2001:23(5):95-103.

    [LIU Hailing, SUN Yan, GUO Lingzhi, et al. On the boundary faults' kinematic characteristics and dynamic process of Nansha ultra-crust layer-block[J]. Acta Geologica Sinica (English edition), 1999,73(4):452-463.]
    [67]
    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.
    [68]
    Huang C H, Xia K Y,Perter B. Structural evolution from Paleogene extension to Latest Miocene Recent arc continent collision offshore Taiwan:comparison with on land geology[J]. Journal of Asian Earth Sciences, 2001,19:619-639.
    [69]
    吴时国,刘文灿.东亚大陆边缘的俯冲带构造[J].地学前缘,2004,11(3):15-22.

    [WU Shiguo, LIU Wencan. Tectonics of subduction zone in the East Asia continental margin[J]. Earth Science Frontiers, 2004, 11(3):15-22.]
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