吉林大学学报(地球科学版) ›› 2016, Vol. 46 ›› Issue (3): 781-797.doi: 10.13278/j.cnki.jjuese.201603114

• 地质与资源 • 上一篇    下一篇

浅谈中国大陆东缘中生代地质演化与泛太平洋板块活动的关系

杨海斌1,2, 田小波1, 白志明1, 张中杰1   

  1. 1. 中国科学院地质与地球物理研究所, 北京 100029;
    2. 吉林大学地球探测科学与技术学院, 长春 130026
  • 收稿日期:2015-11-14 出版日期:2016-05-26 发布日期:2016-05-26
  • 作者简介:杨海斌(1991-),男,研究生,主要从事地球动力学模拟方面的研究,E-mail:sbz522@alumni.ku.dk
  • 基金资助:

    国家自然科学基金项目(41274066);中国科学院地质与地球物理研究所岩石圈演化国家重点实验室项目

Discussion on the Relationship Between Pan Pacific Plate Movement and Mesozoic Geological Evolution of Eastern Chinese Continent

Yang Haibin1,2, Tian Xiaobo1, Bai Zhiming1, Zhang Zhongjie1   

  1. 1. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;
    2. College of Geo-Exploration Science and Technology, Jilin University, Changchun 130026, China
  • Received:2015-11-14 Online:2016-05-26 Published:2016-05-26
  • Supported by:

    Supported by National Natural Science Foundation (41274066) and Projects of State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, CAS

摘要:

本文旨在厘清中生代中国东缘受泛太平洋板块俯冲作用影响下,其可能形成的地质记录的时空分布与泛太平洋板块活动的关系。前者主要从岩浆、构造、沉积盆地的时空演化等角度出发,后者的运动学参数集中在俯冲角度、速度、方向等维度。结果显示:俯冲角度、速度以及方向的改变都有可能形成与之对应的地质事件;但是中国东缘(东北、华北和华南)区域地质记录间的差异也表明,即使都可能遭受俯冲作用,由于个体特殊的构造背景,最终的结果也不尽相同。我们对于中国东缘中、新生代的这一特殊构造现象进行了讨论,得出如下结论:首先三联点力学稳定性分析结果认为,在华北和华南碰撞拼合后,中国大陆东缘可能存在TTT、TTR或者TFT的三联点,而不是简单的稳定的被动大陆边缘;另外,中国华南早、中侏罗世近东西向岩浆岩的形成可能与法拉隆板块和伊泽奈岐板块洋中脊俯冲有关;晚侏罗-早白垩世的板片后撤由NWW向的伊泽奈岐板块与太平洋板块的洋中脊扩张作用所致;而华北克拉通东部记录侏罗纪伊泽奈岐板块俯冲的证据不足,可能并没有发生板块俯冲作用,表现为板块运动与作为中国东部最为薄弱地区的郯庐断裂带的强烈耦合作用。

关键词: 中国大陆东缘, 太平洋板块, 板块俯冲, 中、新生代, 郯庐断裂, 三联点

Abstract:

This paper aims to reveal the relationships between the temperal-spatial distribution of geological recordings, like magmatism, structure and sedimentary basin, and the movement of Pan Pacific plate which intensively influenced the Eastern Chinese continent. As a consequence, variation of plate subducting angle, velocity and direction can produce a great impact on the continent overlying. The Eastern Chinese continent, consisting of Northeast China (NEC), North China(NC) and South China(SC), all were influenced by the Pan Pacific plate subduction on the eastern borde. Due to their various inherent properties, different plates had experienced different geological evolution. Based on discussion on some phenomena characterized as full of anomalies, some conclusions can be drawn for further test. Firstly, through mechanical analysis of possible triple junctions ever existing in eastern China continental frontier, it is suggested that the TTT, TTR or TFT modes should work there, rather than the simplified stable passive continental boundary. Secondly, the origin of west-east distribution of magmatism in central SC might call the ridge of Farallon and Izanagi plate as a reference. The NWW-extending ridge expanding of Izanagi and Pacific could result in the backward movement of plate blocks from the Late Jurassic to Early Cretaceous. Thirdly, few evidence supports the subduction ever took place in the eastern NC, which leads to the hypothesis that the Tanlu fault, the inherent weak part of NC, could have performed as other continent margin, which can be indicated by the strong coupling of plate motion and the corresponding activities of Tanlu fault in Jurassic and Early Cretaceous, instead of plate subduction under NC.

Key words: Eastern Chinese continent, Pacific plate, plate subduction, Mesozoic and Cenozoic, Tanlu fault, triple junctions

中图分类号: 

  • P541

[1] Xiao W J, Windley B F, Hao J, et al. Accretion Leading to Collision and the Permian Solonker Suture, Inner Mongolia, China:Termination of the Central Asian Orogenic Belt[J]. Tectonics, 2003,22(6):1069.

[2] Xiao W J, Windley B F, Huang B C, et al. End Permian to Mid-Triassic Termination of the Southern Central Asian Orogenic Belt[J]. International Journal of Earth Sciences,2009,98:1189-1217.

[3] Li J Y, Gao L M, Sun G H, et al. Shuangjingzi Middle Triassic Syn-Collisional Crust-Derived Granite in the East Inner Mongolia and Its Constraint on the Timing of Collision Between Siberian and Sino-Korean Paleoplates[J]. Acta Petrologica Sinica, 2007, 23:565-582.

[4] 钟大赉. 川滇西部古特提斯造山带[M]. 北京:科学出版社,1998. Zhong Dalai.Paleo-Tethyan Orogenic Belt in Western Sichuan and Western Yunnan[M]. Beijing:Science Press,1998.

[5] Yin A,Harrison T M.Geologic Evolution of the Himalayan-Tibetan Orogen[J].Annual Reviews of Earth and Planet Sci,2000, 28:211-280.

[6] Jaeger J J, Courtillot V, Tapponnier P. Paleontological View of the Ages of the Deccan Traps, the Cretaceous/Tertiary Boundary, and the India-Asia Collision[J]. Geology, 1989, 17:316-319.

[7] 邓晋福, 赵海玲, 莫宣学,等. 大陆根柱构造:大陆动力学的钥匙[M]. 北京:地质出版社, 1996. Deng Jinfu, Zhao Hailing, Mo Xuanxue, et al. Continental Roots-Plume Tectonics:A Key to Continental Dynamics[M]. Beijing:Geological Publishing House, 1996.

[8] 滕吉文,张中杰,王光杰,等.喜马拉雅碰撞造山带的深层动力过程与陆-陆碰撞新模型[J].地球物理学报,1999,42(4):481-494. Teng Jiwen, Zhang Zhongjie, Wang Guangjie, et al. The Deep Internal Dynamical Processes and New Model of Continental-Continental Collision in Himalayan Collision Orogenic Zone[J]. Chinese Journal of Geophysics, 1999, 42(4):481-494.

[9] Zhang Z J, Li Y K, Wang G J, et al. East-West Crust Structure and "Down-Bowing" Moho Under the Northern Tibet Revealed by Wide-Angle Seismic Profile[J]. Science in China:Series D, 2002, 45(6):550-558.

[10] 葛文春,隋振民,吴福元,等. 大兴安岭东北部早古生代花岗岩锆石U-Pb年龄、Hf同位素特征及地质意义[J].岩石学报,2007, 23(2):423-440. Ge Wenchun,Sui Zhenmin,Wu Fuyuan, et al. Hf Isotopic Characteristics and Their Implications of the Early Paleozoic Granites in the Northeastern Da Hinggan Mountains,Northeastern China[J]. Acta Petrologica Sinica,2007,23(2):423-440.

[11] 黑龙江省地质矿产局. 黑龙江省区域地质志[M]. 北京:地质出版社, 1993. Bureau of Geology and Mineral Resources of Heilongjiang Province (BGMRH).Regional Geology of Heilongjiang Province[M]. Beijing:Geological Publishing House,1993.

[12] 刘德来,马莉. 中生代东亚大陆边缘构造演化[J]. 现代地质, 1997,11(4):444-451. Liu Delai, Ma Li. Mesozoic Tectonic Evolution of Continental Margin in East Asia[J]. Geoscience, 1997, 11(4):444-451.

[13] 孙革, 沙金庚,王义刚, 等. 黑龙江饶河东安镇侏罗-白垩系界线及Buchia新知[J].古生物学报,1989, 28(5):579-597. Sun Ge, Sha Jingeng, Wang Yigang, et al. Jurassic-Cretaceous Boundary of Dong'an Zhen, Raohe, Heilongjiang with a New Knowledge of Buchia[J]. Acta Palaeontologica Sinica, 1989, 28(5):579-597.

[14] 水谷申治郎,邵济安,张庆龙. 那丹哈达地体与东亚大陆边缘中生代构造的关系[J].地质学报,1989, 63(3):204-215. Mizutani S, Shao Ji'an, Zhang Qinglong. The Nadanhada Terrene in Relationto Mesozoic Tectonic on Continental Margins of East Asia[J]. Acta Geologica Sinica, 1989, 63(3):204-215.

[15] Zhou J B, Wilde S A, Zhang X Z, et al. The Onset of Pacific Margin Accretion in NE China:Evidence from the Heilongjiang High-Pressure Metamorphic Belt[J].Tectonophysics, 2009, 478(3):230-246.

[16] Li S G, Huang F, Nie Y H, et al. Geochemical and Geochronological Constraints on the Suture Location Between the North and South China Blocks in the Dabie Orogen, Central China[J]. Physics and Chemistry of the Earth, Part A:Solid Earth and Geodesy, 2001, 26(9):655-672.

[17] Carter A, Roques D, Bristow C, et al. Understanding Mesozoic Accretion in Southeast Asia:Significance of Triassic Thermotectonism (Indosinian Orogeny) tn Vietnam[J]. Geology, 2001, 29(3):211-214.

[18] Li Z X, Li X H. Formation of the 1300 km-Wide Intracontinental Orogen and Postorogenic Magmatic Provincein Mesozoic South China:A Flat-Slab Subduction Model[J]. Geology, 2007,35(2):179-182.

[19] 吴根耀,梁兴,陈焕疆.试论郯城-庐江断裂带的形成、演化及其性质[J].地质科学,2007, 42(1):160-175. Wu Genyao, Liang Xing, Chen Huanjiang. An Approach to the Tancheng-Lujiang Fault Zone:Its Creation, Evolution and Character[J]. Chinese Journal of Geology, 2007, 42(1):160-175.

[20] Wu F Y, Yang J H, Wilde S A, et al. Geochronology, Petrogenesis and Tectonic Implications of Jurassic Granites in the Liaodong Peninsula, NE China[J]. Chemical Geology, 2005,221(1):127-156.

[21] Zhu R, Xu Y, Zhu G, et al. Destruction of the North China Craton[J]. Science China Earth Sciences, 55(10):1565-1587.

[22] Maruyama S, Isozaki Y, Kimura G, et al. Paleogeo-graphic Maps of the Japanese Islands:Plate Tectonic Synthesis from 750 Ma to the Present[J]. Island Arc, 2012, 6(1):121-142.

[23] Engebretson D C,Cox A,Gordon R G. Relative Motions Between Oceanic and Continental Plates in the Pacific Basin[M]. Colo:Geological Society of America,1985.

[24] 包汉勇,郭战峰,张罗磊,等.太平洋板块形成以来的中国东部构造动力学背景[J]. 地球科学进展,2013,28(3):337-346. Bao Hanyong, Guo Zhanfeng, Zhang Luolei, et al. Tectonic Dynamics of Eastern China Since the Formation of the Pacific Plate[J]. Advances in Earth Science, 2013, 28(3):337-346.

[25] Koppers A P, Staudigel H, Duncan R A. High-Resolution 40Ar/39Ar Dating of the Oldest Oceanic Basement Basalts in the Western Pacific Basin[J]. Geochemistry Geophysics Geosystems, 2003, 4(11):8914.

[26] Koppers A P,Morgan J P,Morgan J W,et al.Testing the Fixed Hotspot Hypothesis Using 40Ar/39Ar Age Progressions Along Seamount Trails[J].Earth and Planetary Science Letters,2001,185:237-252.

[27] Bartolini A,Larson R L. Pacific Microplate and the Pangea Supercontinent in the Early to Middle Jurassic[J].Geology, 2001,29(8):735-738

[28] Tarduno J A,Cottrell R D. Paleomagnetic Evidence for Motion of the Hawaiian Hotspot During Formation of the Emperor Seamounts[J]. Earth and Planetary Science Letters, 1997, 153(3):171-180.

[29] Northrup C,Royden L,Burchfoel B. 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(8):719-722.

[30] Bedard J H. A Catalytic Delamination-Driven Model for Coupled Genesis of Archaean Crust and Sub-Continental Lithospheric Mantle[J]. Geochimica et Cosmochimica Acta, 2006, 70:1188-1214.

[31] Espurt N, Funiciello F, Martinod J, et al. Flat Subduc-tion Dynamics and Deformation of the South American Plate:Insights from Analog Modeling[J]. Tectonics, 2008, 27(3):1-19.

[32] Li X H, Li Z X, Li W X, et al. Initiation of the Indo-sinian Orogeny in South China:Evidence for a Permian Magmatic Arc on Hainan Island[J]. The Journal of Geology, 2006,114:341-353, doi:10.1086/501222.

[33] Wang Q, Li J W, Jian P, et al. Alkaline Syenites in Eastern Cathaysia (South China):Link to Permian-Triassic Transtension[J]. Earth and Planetary Science Letters, 2005, 230:339-354, doi:10.1016/j.epsl.2004.11.023.

[34] Livaccari R F, Burke K, Seng r A M C. Was the Laramide Orogeny Related to Subduction of an Oceanic Plateau?[J]. Nature, 1981, 289:276-278.

[35] Li J, Zhang Y, Dong S, et al. Cretaceous Tectonic Evolution of South China:A Preliminary Synthesis[J]. Earth-Science Reviews, 2014, 134:98-136.

[36] Kimura T. Geographical Distribution of Paleozoic and Mesozoic Plants in East and Southeast Asia[M]//Taira A,Tashiro M.Historical Biogeography and Plate Tectonic Evolution of Japan and Eastern Asia. Tokyo:Terra Sci Pub,1987:135-200.

[37] Hayamii. Geographic Distribution of Jurassic Bivalve Faunas in Eastern Asia[C]//Ichikawa K, Mizutani S, Hara I, et al. Pre-Cretaceous Terranes of Japan.Osaka:Publication of ICGP Project 224,1990:361-369.

[38] Wu F Y, Sun D Y, Ge W C, et al. Geochronology of the Phanerozoic Granitoids in Northeastern China[J]. Journal of Asian Earth Sciences, 2011, 41(1):1-30.

[39] Zhang J H, Gao S, Ge W C,et al. Geochronology of the Mesozoic Volcanic Rocks in the Great Xing'an Range, Northeastern China:Implications for Subduction-Induced Delamination[J]. Chemical Geology, 2010, 276(3):144-165.

[40] Xu W L, Pei F P, Wang F, et al. Spatial-Temporal Relationships of Mesozoic Volcanic Rocks in NE China:Constraints on Tectonic Overprinting and Transforma-tions Between Multiple Tectonic Regimes[J]. Journal of Asian Earth Sciences, 2013, 74:167-193.

[41] Zhou X M,Li W X. Origin of Late Mesozoic Igneous Rocks in Southeastern China:Implications for Lithosphere Subduction and Underplating of Mafic Magmas[J]. Tectonophysics, 2000,326(3):269-287.

[42] Chen P R,Hua R M, Zhang B T, et al. Early Yanshanian Post-Orogenic Granitoids in the Nanling Range Region:Petrological Constraints and Geodynamic Settings[J]. Science in China:Series D:Earth Sciences, 2002,48(8):755-768.

[43] Zhai M, Zhu R, Liu J,et al. Time Range of Mesozoic Tectonic Regime Inversion in Eastern North China Block[J]. Science in China:Series D:Earth Sciences, 2004, 47(2):151-159.

[44] 刘红涛,翟明国,刘建明,等. 华北克拉通北缘中生代花岗岩:从碰撞后到非造山[J].岩石学报,2002, 48(4):433-448. Liu Hongtao, Zhai Mingguo, Liu Jianming, et al. The Mesozoic Granitoids in the Northern Marginal Region of North China Craton:Evolution from Post-Collisional to Anorogenic Settings[J]. Acta Petrologica Sinica, 2002,18(4):433-448.

[45] 吴福元,李献华,杨进辉,等.花岗岩研究的若干问题[J].岩石学报, 2007,23(6):1217-1238. Wu Fuyuan, Li Xianhua, Yang Jinhui, et al. Discussions on the Petrogenesis of Graites[J]. Acta Petrologica Sinica, 2007, 23(6):1217-1238.

[46] Zhou X M, Sun T, Shen W, et al. Petrogenesis of Mesozoic Granitoids and Volcanic Rocks in South China:A Response to Tectonic Evolution[J].Episodes, 2006, 29(1):26.

[47] 周新民.对华南花岗岩研究的若干思考[J]. 高校地质学报,2003, 9(4):556-565. Zhou Xinmin. My Thinking About Granite Geneses of South China[J]. Geological Journal of China Universities,2003, 9(4):556-565.

[48] Wang F, Zhou X H, Zhang L C, et al. Late Mesozoic Volcanism in the Great Xing'an Range (NE China):Timing and Implications for the Dynamic Setting of NE Asia[J]. Earth and Planetary Science Letters, 2006, 251(1):179-198.

[49] Xu Y, Li H, Pang C, et al. On the Timing and Dura-tion of the Destruction of the North China Craton[J]. Chinese Science Bulletin, 2009,54(19):3379-3396.

[50] Zhang S H, Zhao Y, Davis G A, et al. Temporal and Spatial Riations of Mesozoic Magmatism and Deformation in the North China Craton:Implications for Lithospheric Thinning and Decratonization[J]. Earth-Science Reviews, 2014, 131:49-87.

[51] 朱光,胡召齐,陈印,等.华北克拉通东部早白垩世伸展盆地的发育过程及其对克拉通破坏的指示[J].地质通报,2008, 27(10):1594-1604. Zhu Guang, Hu Zhaoqi, Chen Yin, et al. Evolution of Early Cretaceous Extensional Basins in the Eastern North Chinacraton and Its Implication for the Craton Destruction[J]. Geological Bulletin of China, 2008, 27(10):1594-1604.

[52] 张庆龙,王良书,解国爱,等. 郯庐断裂带北延及中新生代构造体制转换问题的探讨[J]. 高校地质报, 2005,11(4):577-584. Zhang Qinglong, Wang Liangshu, Xie Guoai, et al. Discussion on Northward Extension of the Tanlu Fault Zone and Its Tectonic Regime Transformation[J].Geological Journal of China Universities,2005,11(4):577-584.

[53] 徐嘉炜. 郯-庐断裂带巨大的左行平移运动[J].合肥工业大学学报,1980(1):1-26. Xu Jiawei. The Horizontal Displacement of Tancheng-Lujiang Fault Zone and Its Geological Significance[J]. Journal of Hefei University of Techndogy,1980(1):1-26.

[54] 张岳桥,董树文. 郯庐断裂带中生代构造演化史:进展与新认识[J]. 地质通报,2008, 27(9):1371-1390. Zhang Yueqiao, Dong Shuwen.Mesozoic Tectonic Evolution History of the Tan-Lu Fault Zone, China:Advances and New Understanding[J]. Geological Bulletin of China, 2008,27(9):1371-1390.

[55] Wang Y. The Onset of the Tan-Lu Fault Movement in Eastern China:Constraints from Zircon (SHRIMP) and 40Ar/39Ar Dating[J]. Terra Nova, 2006, 18:423-431.

[56] 万天丰,朱鸿. 郯庐断裂带的最大左行走滑断距及其形成时期[J].高校地质学报,1996, 2(1):14-27. Wan Tianfeng, Zhu Hong.The Maximum Sinistral Strike-Slip and Its Forming Age of Tancheng-Lujiang Fault Zone[J]. Geological Journal of Universities, 1996, 2(1):14-27.

[57] 朱光,王道轩,刘国生,等. 郯庐断裂的伸展活动及其动力学背景[J]. 地质科学,2001, 36(3):269-278. Zhu Guang, Wang Daoxuan, Liu Guosheng, et al. Extensional Activities Along the Tan-Lu Fault Zoneand Its Geodynamic Setting[J]. Chinese Journal of Geology,2001, 36(3):269-278.

[58] 侯贵廷,冯大晨,王文明,等. 松辽盆地的反转构造作用及其对油气成藏的影响[J].石油与天然气地质,2004, 25(1):49-53. Hou Guiting, Feng Dachen, Wang Wenming, et al.Revese Structures and Their Impacts on Hydrocarbon Accumulation in Songliao Basin[J]. Oil & Gas Geology, 2004, 25(1):49-53.

[59] 孙晓猛,王书琴,王英德,等. 郯庐断裂带北段构造特征及构造演化序列[J].岩石学报,2010, 26(1):165-176. Sun Xiaomeng, Wang Shuqin, Wang Yingde, et al. The Structural Feature and Evolution Series in the Northern Segment of Tancheng-Lujiang Fault Zone[J]. Acta Petrologica Sinica, 2010, 26(1):165-176.

[60] 舒良树,周新民. 中国东南部晚古中生代构造作用[J]. 地质论评, 2002, 48(3):249-260. Shu Liangshu, Zhou Xinmin. Late Mesozoic Tectonism of Southeast China[J].Geological Riview, 2002,48(3),249-260.

[61] 江博明, 刘忠光.台湾蓝闪石片岩的年龄与其对构造环境的追认所受的地球化学的约束[J]. 台湾地质学会会刊, 1977(2):129-140. Jahn Boming, Liu Zhongguang. Age and Geochemical Constraints of Glaucophane Schists of Taiwan[J]. Mern Geol Soc China,1977(2):129-140.

[62] Lo C H, Yui T H. 40Ar/39Ar Dating of High-Pressure Rocks in the Tananao Basement Complex[J]. Taiwan J Geol Soc China, 1996, 39(1):13-30.

[63] Kearey P, Klepeis K A, Vine F J. Global Tectonics[M]. Oxford:John Wiley & Sons, 2009:113-120.

[64] Gilder S A, Leloup P H, Courtillot V, et al. Tectonic Evolution of the Tancheng-Lujiang (Tan-Lu) Fault via Middle Triassic to Early Cenozoic Paleomagnetic Data[J]. Journal of Geophysical Research:Solid Earth (1978-2012), 1999, 104(B7):15365-15390.

[65] 李三忠,余珊,赵淑娟,等. 东亚大陆边缘的板块重建与构造转换[J]. 海洋地质与第四纪地质,2013,3(33):65-94. Li Sanzhong, Yu Shan, Zhao Shujian, et al. Tectonic Transition and Plate Reconstructions of the East Asian Continental Magin[J]. Marine Geology & Quaternary Geology, 2013, 3(33):65-94.

[66] Deng Y, Zhang Z, Fan W, et al. Multitaper Spectral Method to Estimate the Elastic Thickness of South China:Implications for Intracontinental Deformation[J]. Geoscience Frontiers, 2014, 5(2):193-203.

[67] Maruyama S, Santosh M, Zhao D. Superplume, Super-continent, and Post-Perovskite:Mantle Dynamics and Anti-Plate Tectonics on the Core-Mantle Boundary[J]. Gondwana Research, 2007, 11(1):7-37.

[68] Van der Hilst R D, Widiyantoro S, Engdahl E R. Evi-dence for Deep Mantle Circulation from Global Tomography[J]. Nature, 1997, 386(6625):578-584.

[69] Grand S P, Van der Hilst R D, Widiyantoro S. Global Seismic Tomography:A Snapshot of Convection in the Earth[J]. GSA Today, 1997, 7(4):1-7.

[70] Bedard J H, Harris L B, Thurston P C. The Hunting for the Snarc[J]. Precambrian Research, 2013, 229:20-48.

[71] Sun W, Ding X, Hu, Y H, et al. The Golden Trans-formation of the Cretaceous Plate Subduction in the West Pacific[J]. Earth and Planetary Science Letters, 2007, 262(3), 533-542.

[72] Li J, Yuen D A. Mid-Mantle Heterogeneities Associated with Izanagi Plate:Implications for Regional Mantle Viscosity[J]. Earth and Planetary Science Letters, 2014,385:137-144.

[73] Huang J,Zhao D. High-Resolution Mantle Tomography of China and Surrounding Regions[J]. Journal of Geophysical Research:Solid Earth(1978-2012), 2006, 111(B9):1-21.

[74] 臧绍先, 宁杰远. 西太平洋俯冲带的研究及其动力学意义[J]. 地球物理学报,1996, 39(2):188-202. Zang Shaoxian, Ning Jieyuan. Study on the Subduction Zone in Western Pacific and Its Implication for the Geodynamics[J]. Chinaese Journal Geophysics, 1996, 39(2):188-202.

[75] Xu Y G, Zhang, H H, Qiu, H N,et al. Oceanic Crust Components in Continental Basalts from Shuangliao, Northeast China:Derived from the Mantle Transition Zone?[J]. Chemical Geology, 2012, 328:168-184.

[76] 徐义刚.太行山重力梯度带的形成与华北岩石圈减薄的时空差异性有关[J].地球科学:中国地质大学学报,2006,31(1):14-22. Xu Yigang. Formation of the Taihangshan Gravity Linement by the Diachronous Lithospheric Thinning of the North China Craton[J]. Earth Science:Journal of China Universities of Geosciences, 2006, 31(1):14-22.

[77] Liu L, Spasojevic S, Gurnis M. Reconstructing Farallon Plate Subduction Beneath North America Back to the Late Cretaceous[J]. Scinece, 2008,322:934-937.

[78] Liu L, Stegman D R. Origin of the Columbia River Flood Basalt Controlled by Propagating Rupture of the Farallon Slab[J]. Nature, 2012, 482:386-392.

[79] 张岳桥,赵越,董树文,等. 中国东部及邻区早白垩世裂陷盆地构造演化特征[J]. 地学前缘,2004, 11(3):123-133. Zhang Yueqiao, Zhao Yue, Dong Shuwen, et al.Tectonic Evolution Stages of the Early Cretaceous Rift Basins in Eastern China and Adjacent Areas and Their Geodynamic Background[J]. Earth Science Frontiers, 2004,11(3):124-133.

[80] Larson R L. Geological Consequences of Superplumes[J]. Geology,1991,19(10):963-966.

[81] Tissot B. Effects on Prolifi C Petroleum Source Rocks and Major Coal Deposits Caused by Sea-Level Changes[J]. Nature,1979, 277:463-465.

[1] 张超, 崔芳华, 张照录, 耿瑞, 宋明春. 鲁西金岭地区含矿闪长岩体成因:来自锆石U-Pb年代学和地球化学证据[J]. 吉林大学学报(地球科学版), 2017, 47(6): 1732-1745.
[2] 陈井胜, 李崴崴, 刘淼, 邢德和, 杨佳林. 辽西建平马场义县组火山岩LA-ICP-MS锆石U-Pb年龄及其地质意义[J]. 吉林大学学报(地球科学版), 2015, 45(2): 471-482.
[3] 高万里,王宗秀,王对兴,李春麟. 浙东南晚中生代花岗岩的锆石U-Pb年代学、地球化学及其地质意义[J]. 吉林大学学报(地球科学版), 2014, 44(3): 861-875.
[4] 黄超,余朝华,张桂林,傅良同,袁志云,范兴燕. 郯庐断裂中段新生代右行走滑位移[J]. 吉林大学学报(地球科学版), 2013, 43(3): 820-832.
[5] 彭向东, 李蔚伟, 李晓敏, 石春磊. 黑龙江省嘉荫县乌拉嘎断陷中、新生代地层序列与盆地演化[J]. J4, 2011, 41(1): 86-92.
[6] 赵院冬, 迟效国, 车继英, 刘建峰, 赵芝. 延边-东宁地区晚三叠世花岗岩地球化学特征及其大地构造背景[J]. J4, 2009, 39(3): 425-434.
[7] 孙晓猛,刘永江,孙庆春,韩国卿,王书琴,王英德. 敦密断裂带走滑运动的40Ar/39Ar年代学证据[J]. J4, 2008, 38(6): 965-0972.
[8] 江 涛,邱玉超,王立武,宋立忠,苗洪波,丁 冶. 伊通盆地二号断层与西拉木伦河断裂带及油气的关系[J]. J4, 2008, 38(3): 411-0416.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!