Regional Background and Tectonic Evolution of East China Sea Basin
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摘要: 东海盆地处于西太平洋俯冲带前缘，是发育在华南克拉通基底之上的，以晚白垩世-新生代沉积为主的新生代盆地.东海盆地性质是在活动大陆边缘减薄陆壳之上的，由于洋-陆俯冲消减所引起的张裂、拉伸作用而形成的弧后裂谷型盆地，是西太平洋众多“沟-弧-盆”体系的一部分.东海盆地陆架外缘隆起控制着东海盆地的演化过程，该地质单元形成于晚白垩世，是陆缘隆起和增生楔的复合体，中新世后由于菲律宾海板块的活动而解体为现今的钓鱼岛隆褶带和琉球隆起.结合对陆架外缘隆起的研究后认为，东海盆地晚白垩世以来的演化历程具有3大构造阶段，即：第一阶段，古新世-中始新世西部坳陷形成发展期；第二阶段，中始新世-渐新世东部坳陷形成发展期，其中，中晚始新世太平洋板块的转向是东、西部坳陷构造迁移的分界点；第三阶段，中新世-全新世，东海盆地进入到菲律宾板块影响时期，原先的构造格局开始分解.Abstract: The East China Sea Basin that located in the front of the west Pacific subduction zone, is formed upon the Huanan Craton basement. The main sediment filling are from Late Cretaceous to Cenozoic. The East China Sea Basin developed on the thinned continental margin crust, is a back-arc rift basin caused by rifting and stretching that induced by ocean subduction, which is the part of the "trench-arc-basin" system in the west Pacific. The tectonic evolution was controlled by the uplift in the outer continental shelf that formed in the Late Cretaceous. The uplift is the complex of the continental margin uplift and accretionary wedge that disintegrated into Diaoyu Island fold belt and Ryukyu uplift after Miocene. Considering the study of the outer continental shelf uplift, tectonic evolution history of the East China Sea basin after Late Cretaceous can be divided into three stages: the first stage, the Paleocene to Middle Late Eocene, formation and development of the western depression; the second stage, Middle Late Eocene to Oligocene, formation and development of the eastern depression, in which the rotary of the Pacific plate boundary in the Middle Late Eocene is the demarcation point of the tectonic migration of the eastern depression and western depression; the third stage, Miocene-Holocene, impaction of the Philippine Sea Plate period, the original structure pattern of the East China Sea Basin began to decompose.
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Key words:
- East China Sea basin /
- basin type /
- back arc rift basin /
- tectonics
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图 1 东海盆地及临区构造地质纲要
Fig. 1. Structural geology outline map of East China Sea basin and adjacent area
图 3 东海盆地火山岩主量元素三角图解
据Mullen(1983)修改；OIT.大洋拉斑玄武岩；CAB.岛弧钙碱性玄武岩；IAT.岛弧拉斑玄武岩；OIA.碱性玄武岩；Tholeiitic.拉斑玄武岩；Calc-Alkaline.钙碱性玄武岩
Fig. 3. The triangular diagram of volcanic major elements in East China Sea basin
图 4 东海盆地花岗岩构造环境判识图
Fig. 4. The granite tectonic environment discrimination in East China Sea basin FM=FeO+MgO; C=CaO; R1=4Si-11(Na+K)-2(Fe+Ti); R2=6Ca+2Mg+Al
图 5 太平洋板块与中国近海盆地形成的关系
据Watson et al.(1987); Northrup et al.(1995)修改
Fig. 5. The Pacific plate's relationship with China offshore basins
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An, M.J., Zhao, Y., Feng, M., et al., 2011.What Resulted in New Tectonic Activities in the Eastern North China Craton in the Neogene?Earth Science Frontiers, 18(3):121-140 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY201103014.htm Clague, D.A., Dalrymple, G.B., 1987.Geologic Evolution of the Hawaiian-Emperor Volcanic Chain.US Geological Survey Professional Paper, 1350:5-54. Cui, S.Q., Li, J.R., 1990.Himalayan Tectonic Evolution in the Peri-Pacific Region of East Asia.Acta Geologica Sinica, 64(1):1-12 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE199001000.htm Fang, Y.X., Liu, J.H., 2004.The Crustal Structure Character of East China Sea.Donghai Marine Science, 22(3):9-17 (in Chinese with English abstract). http://www.cqvip.com/QK/71135X/201107/20307216.html Gao, D.Z., Tang, J., Bo, Y.L., 2003.An Integrated Profile of Geophysical Survey and its Interpretation in East China Sea.China Offshore Oil and Gas, (1):40-45 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZHSD200301007.htm Hilde, T.W.C., Uyeda, S., Kroenke, L., 1977.Evolution of the Western Pacific and its Margin.Tectonophysics, 38(1-2):145-165.doi: 10.1016/0040-1951(77)90205-0 Hu, H.J., Tao, G.B., 1997.Tertiary Magmatism and its Relationaship with Oil/gas Accumulation in the Xihu Sag, the East China Sea.Offshore Oil, (3):13-19 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HYSY199703002.htm Jin, X.L., Yu, P.Z., 1987.Structural Characteristics and Evolution of the Okinawa Trough.Science in China (Series.B), (2):196-203 (in Chinese). Kimura Masaaki, Wang, Y.G., Yagi Hideken, 1999.The development history of the geological structure of the Ryukyu Arc.Geological News Scan, 11(543):24-38 (in Japanese). Kong, F.C., Lawver, L.A., Lee, T.Y., 2000.Evolution of the Southern Taiwan-Sinzi Folded Zone and Opening of the Southern Okinawa Trough.Journal of Asian Earth Sciences, 18(3):325-341.doi: 10.1016/s1367-9120(99)00062-0 Lee, J.S., 1939.The Geology of China.Murby, USA. Li, N.S., Jiang, L.L., Li, C.Z., 1998.A Study on the Nature of Crustal Structures of the Okinawa Trough.Oceanologia et Limnologia Sinica, 29(4):441-450 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HYFZ199804015.htm Li, S.Z., Zhang, G.W., Zhou, L.H., et al., 2011.The Opposite Meso-Cenozoic Intracontinental Deformations under the Superconvergence:Rifting and Extension in the North China Craton and Shortening and Thrusting in the South China Craton.Earth Science Frontiers, 18(3):79-107 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DXQY201103012.htm Li, Y.L., Zhou, H.W., Xiao, W.J., et al., 2012.Superposition of Paleo-Asian and West-Pacific Tectonic Domains in the Eastern Section of the Solonker Suture Zone:Insights from Petrology, Geochemistry and Geochronology of Deformed Diorite in Xar Moron Fault Zone, Inner Mongolia.Earth Science, (3):433-450 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX201203008.htm Liu, G.D., 1992.Geological and Geophysical Characteristics of China Sea Area and Its Adjacent Areas.Sciences Press, Beijing (in Chinese). Liu, H.F., 1993.Dynamic Classification of Sedimentary Basins and Their Structure Styles.Earth Science, 18(6):699-724 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX199306006.htm Liu, J.J., Chen, K.Y., Shi, Z.S., et al., 2003.Provenance Analysis of the Lower Three Series in the West Lake Depression of the East China Sea Shelf Basin.Science & Technology Progress and Policy, 20(S1):241-242 (in Chinese). Liu, S.S., Li, S.Q., 2001.Geophysical Exploration of Oil and Gas in the East China Sea.Geological Publishing House, Beijing, 91-92 (in Chinese). Luo, M.S., Lu, L.Q., Jia, J., et al., 2014.Evolution of Sedimentary Basins in China during Mesozoic.Earth Science, 39(8): 954-976 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX201408003.htm Miyashiro, A., 1973.Paired and Unpaired Metamorphic Belts.Tectonophysics, 17(3):241-254.doi: 10.1016/0040-1951(73)90005-x Mullen, E.D., 1983.MnO/TiO2/P2O5:A Minor Element Discriminant for Basaltic Rocks of Oceanic Environments and its Implications for Petrogenesis.Earth and Planetary Science Letters, 62(1):53-62.doi: 10.1016/0012-821x(83)90070-5 Northrup, C.J., Royden, L.H., Burchfiel, B.C., 1995.Motion of the Pacific Plate Relative to Eurasia and Its Potential Relation to Cenozoic Extension along the Eastern Margin of Eurasia.Geology, 23(8):719.doi:10.1130/0091-7613(1995)023<0719:motppr>2.3.co;2 Ren, J.W., Ma, Z.J., 2003.Crustal Movement and Tectonic Deformation of Eastern Asia.Earth Science Frontiers, 10(Z1):58-65 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY2003S1010.htm Richards, M.A., Lithgow-Bertelloni, C., 1996.Plate Motion Changes, the Hawaiian-Emperor Bend, and the Apparent Success and Failure of Geodynamic Models.Earth and Planetary Science Letters, 137(1-4):19-27.doi: 10.1016/0012-821x(95)00209-u Sun, Z.C., 2004.Progress of Petroleum Geology Research for the East China Sea and on Tectonic Evolution of Cenozoic Basins in the Continental Margins along the West Pacific Ocean:An Evolutional Model of Oceanwards-Receding Residual Rear-Arc Basins.Marine Origin Petoleum Geology, 9(Z1):1-17, 124 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-HXYQ2004Z1001.htm Wang, G.C., 1987.Formation and Evolution of the East China Sea Basin.Acta Petrolei Sinica, 8(4):18-25 (in Chinese with English abstract). http://www.syxb-cps.com.cn/EN/Y1987/V8/I4/18 Wang, L.F., Wang, J.Y., 2006.A Geothermal Study of Gas Hydrates in the East China Sea and Its Environmental Implications.Earth Science Frontiers, 13(1):15-20 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY200601001.htm Watson, M.P., Hayward, A.B., Parkinson, D.N., et al., 1987.Plate Tectonic History, Basin Development and Petroleum Source Rock Deposition Onshore China.Marine and Petroleum Geology, 4(3):205-225.doi: 10.1016/0264-8172(87)90045-6 Xu, J., Zhou, B.G., Ji Feng (jie|ju), et al., 2012.The Recent Tectonic Stress Field of Offshore of China Mainland and Adjacent Areas.Earth Science Frontiers, 19(4):1-7 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY201204001.htm Xu, Y.D., Liang, Y.P., Jiang, S.S., et al., 2014.Evolution of Cenozoic Sedimentary Basins in Eastern China.Earth Science, 39(8):1079-1098 (in Chinese with English abstract). Yang, X.H., Li, A.C., 2003.Basement Nature and Sedimentary Basins along the Continental Margin in East China Sea.China Offshore Oil and Gas:Geology, 17(1):25-28, 56 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZHSD200301004.htm Zhang, Y.Q., Xu, X.B., Jia, D., et al., 2009.Deformation Record of the Change from Indosinian Collision-Related Tectonic System to Yanshanian Subduction-Related Tectonic System in South China during the Early Mesozoic.Earth Science Frontiers, 16(1):234-247 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY200901033.htm Zhou, Z.W., Zhao, J.H., Yin, P.L., 1990.Structural Features and Hydrocarbon Bearing Characteristics of the Shelf Basin of the East China Sea.In: Zhu, X., Xu, W., eds., Mesozoic and Cenozoic Sedimentary Basins in China.Petroleum Industry Press, Beijing, 226-242 (in Chinese). Zhou, Z.Y., Liao, Z.T., Jin, X.C., et al., 2001.Okinawa Trough:The Highest Stage of Continental Tension Rifting in Back-Arc Setting.Marine Geology & Quaternary Geology, 21(1):51-55 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HYDZ200101009.htm 安美建, 赵越, 冯梅, 等, 2011.什么控制了华北克拉通东部在新近纪的构造活动?地学前缘, 18(3): 121-140. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201103014.htm 崔盛芹, 李锦蓉, 1990.东亚滨太平洋地区喜马拉雅期构造演化.地质学报, 64(1): 1-12. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE199001000.htm 方银霞, 刘建华, 2004.东海的地壳结构特征.东海海洋, 22(3): 9-17. http://www.cnki.com.cn/Article/CJFDTOTAL-DHHY200403002.htm 高德章, 唐建, 薄玉玲, 2003.东海地球物理综合探测剖面及其解释.中国海上油气.地质, (1): 40-45. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGDW200210001209.htm 胡惠娟, 陶国保, 1997.东海西湖凹陷第三纪岩浆活动与油气聚集的关系.海洋地质译丛, (3): 13-19. http://www.cnki.com.cn/Article/CJFDTOTAL-HYSY199703002.htm 金翔龙, 喻普之, 1987.冲绳海槽的构造特征与演化.中国科学:B辑, (2): 196-203. http://cdmd.cnki.com.cn/Article/CDMD-10423-1014368502.htm 李乃胜, 姜丽丽, 李常珍, 1998.冲绳海槽地壳结构的研究.海洋与湖沼, 29(4): 441-450. http://www.cnki.com.cn/Article/CJFDTOTAL-HYFZ199804015.htm 李三忠, 张国伟, 周立宏, 等, 2011.中、新生代超级汇聚背景下的陆内差异变形:华北伸展裂解和华南挤压逆冲.地学前缘, 18(3): 79-107. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201103012.htm 李益龙, 周汉文, 肖文交, 等, 2012.古亚洲构造域和西太平洋构造域在索伦缝合带东段的叠加:来自内蒙古林西县西拉木伦断裂带内变形闪长岩的岩石学、地球化学和年代学证据.地球科学, 37(3): 433-450. http://earth-science.net/WebPage/Article.aspx?id=2248 刘光鼎, 1992.中国海区及邻域地质地球物理特征.北京:科学出版社. 刘和甫, 1993.沉积盆地地球动力学分类及构造样式分析.地球科学, 18(6): 699-814. http://earth-science.net/WebPage/Article.aspx?id=85 刘建军, 陈开远, 史忠生, 等, 2003.东海陆架盆地西湖凹陷下第三系物源分析.科技进步与对策, 20(S1): 241-242. http://www.cnki.com.cn/Article/CJFDTOTAL-KJJB2003S1122.htm 刘申叔, 李上卿, 2001.东海油气地球物理勘探.北京:地质出版社, 91-92. 骆满生, 卢隆桥, 贾建, 等, 2014.中国中生代沉积盆地演化.地球科学, 39(8): 954-976. http://earth-science.net/WebPage/Article.aspx?id=2912 木村政昭, Wang Yugang, 八木秀憲, 1999.琉球弧海域の海底地質構造ぉょぴ發達史.地質ニュ?ス543号, 11: 24-38. 任金卫, 马宗晋, 2003.东亚地区现代地壳运动特征与构造变形.地学前缘, 10(z1): 58-65. doi: 10.3321/j.issn:1005-2321.2003.z1.011 孙肇才, 2004.从东海石油地质重要进展看西太平洋大陆边缘新生代盆地的构造演化——一种海沟向洋后退的残余弧后盆地演化模式.海相油气地质, 9(Z1): 1-17, 124. http://www.cnki.com.cn/Article/CJFDTOTAL-SYSD200402003.htm 王国纯, 1987.东海陆架盆地的形成与演化.石油学报, 8(4): 18-25. doi: 10.7623/syxb198704003 王力锋, 汪集旸, 2006.东海天然气水合物地热研究及其环境意义.地学前缘, 13(1): 15-20. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200601001.htm 徐杰, 周本刚, 计凤桔, 等, 2012.中国东部海域及其邻区现代构造应力场研究.地学前缘, 19(4): 1-7. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201204001.htm 徐亚东, 梁银平, 江尚松, 等, 2014.中国东部新生代沉积盆地演化.地球科学, 39(8): 1079-1098. http://earth-science.net/WebPage/Article.aspx?id=2918 杨香华, 李安春, 2003.东海大陆边缘基底性质与沉积盆地.中国海上油气:地质, 17(1): 25-28, 56. http://www.cnki.com.cn/Article/CJFDTOTAL-ZHSD200301004.htm 张岳桥, 徐先兵, 贾东, 等, 2009.华南早中生代从印支期碰撞构造体系向燕山期俯冲构造体系转换的形变记录.地学前缘, 16(1): 234-247. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200901033.htm 周志武, 赵金海, 殷培龄, 1990. 东海陆架盆地构造特征及含油气性. 见: 朱夏, 徐旺主编. 中国中新生代沉积盆地. 北京: 石油工业出版社, 226-242. 周祖翼, 廖宗廷, 金性春, 等, 2001.冲绳海槽——弧后背景下大陆张裂的最高阶段.海洋地质与第四纪地质, 21(1): 51-55. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200101009.htm -
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