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

奥陶纪到志留纪全球板块重建:中国三大陆块位置及其洋陆格局的运动学检验

聂仕琪 黄金水 李三忠

聂仕琪, 黄金水, 李三忠. 奥陶纪到志留纪全球板块重建:中国三大陆块位置及其洋陆格局的运动学检验[J]. 海洋地质与第四纪地质, 2015, 35(4): 177-188. doi: 10.16562/j.cnki.0256-1492.2015.04.019
引用本文: 聂仕琪, 黄金水, 李三忠. 奥陶纪到志留纪全球板块重建:中国三大陆块位置及其洋陆格局的运动学检验[J]. 海洋地质与第四纪地质, 2015, 35(4): 177-188. doi: 10.16562/j.cnki.0256-1492.2015.04.019
NIE Shiqi, HUANG Jinshui, LI Sanzhong. GLOBAL PLATE RECONSTRUCTION FROM ORDIVICIAN TO SILURIAN: KINEMATICS TEST OF THEIR LOCATIONS OF THREE CHINA'S CONTINENTS AND OCEAN-CONTINENT CONFIGURATION[J]. Marine Geology & Quaternary Geology, 2015, 35(4): 177-188. doi: 10.16562/j.cnki.0256-1492.2015.04.019
Citation: NIE Shiqi, HUANG Jinshui, LI Sanzhong. GLOBAL PLATE RECONSTRUCTION FROM ORDIVICIAN TO SILURIAN: KINEMATICS TEST OF THEIR LOCATIONS OF THREE CHINA'S CONTINENTS AND OCEAN-CONTINENT CONFIGURATION[J]. Marine Geology & Quaternary Geology, 2015, 35(4): 177-188. doi: 10.16562/j.cnki.0256-1492.2015.04.019

奥陶纪到志留纪全球板块重建:中国三大陆块位置及其洋陆格局的运动学检验


doi: 10.16562/j.cnki.0256-1492.2015.04.019
详细信息
    作者简介:

    聂仕琪(1989-),男,硕士,从事板块构造与地球动力学研究,Email:nsq@mail.ustc.edu.cn

  • 基金项目:

    国家自然科学基金项目(91014005,41474082)

    国家自然科学基金重大项目(41190072)

  • 中图分类号: P736.1

GLOBAL PLATE RECONSTRUCTION FROM ORDIVICIAN TO SILURIAN: KINEMATICS TEST OF THEIR LOCATIONS OF THREE CHINA'S CONTINENTS AND OCEAN-CONTINENT CONFIGURATION

More Information
  • 摘要: 中国三大陆块是全球奥陶纪到志留纪板块与洋陆格局重建的关键,涉及到古亚洲洋与原特提斯洋的演化。综合了全球奥陶纪到志留纪的古地磁、古生物、古气候以及地球化学的相关证据,重建了中国三大陆块在这一时期的板块演化与洋陆格局,并将它们与全球板块演化模型结合到一起,特色在于通过板块运动的速度场分析,厘定了全球重要的板块边界及其性质。得到以下新认识:在奥陶纪到志留纪,中国三大陆块独立地位于地球的低纬地区,并且不依附于任何大的陆块,离散分布于原特提斯洋与古亚洲洋之间,原特提斯洋与古亚洲洋不断消减俯冲。其中,华北陆块早期靠近西伯利亚大陆东缘,华南陆块在奥陶纪早期沿着冈瓦纳大陆西侧漂移,塔里木陆块在奥陶纪进行了一个南北向的大范围的运动后,在志留纪开始向西漂移。中国三大陆块在这一时期不断地相互作用。在奥陶纪到中志留纪,原特提斯洋不断地俯冲冈瓦纳大陆与华北大陆,直到晚志留纪,随着古特提斯洋的扩张,原特提斯洋开始逐渐闭合。
  • [1] Scotese CR, McKerrow WS. Revised world maps and introduction[J]. Geological Society, London, Memoirs, 1990, 12:1-21.
    [2] Metcalfe I. Palaeozoic-mesozoic history of se asia[J]. Geological Society, London, Special Publications, 2011, 355:7-35.
    [3] Stampfli G, Hochard C, Vérard C, et al. The formation of pangea[J]. Tectonophysics, 2013, 593:1-19.
    [4] Torsvik TH, Steinberger B, Cocks LRM, et al. Longitude:Linking earth's ancient surface to its deep interior[J]. Earth and Planetary Science Letters, 2008, 276:273-282.
    [5] Seton M, Müller R, Zahirovic S, et al. Global continental and ocean basin reconstructions since 200 Ma[J]. Earth-Science Reviews, 2012, 113:212-270.
    [6] Domeier M, Torsvik TH. Plate tectonics in the late paleozoic[J]. Geoscience Frontiers, 2014, 5:303-350.
    [7] Torsvik TH, van der Voo R, Doubrovine PV, et al. Deep mantle structure as a reference frame for movements in and on the earth[J]. Proceedings of the National Academy of Sciences, 2014, 201318135.
    [8] Cocks, L.R.M., Torsvik, T.H. The dynamic evolution of the Palaeozoic geography of eastern Asia[J]. Earth-Science Reviews,2013,117, 40-79.
    [9] Cocks LRM, Torsvik TH. The palaeozoic geography of laurentia and western laurussia:A stable craton with mobile margins[J]. Earth-Science Reviews, 2011, 106:1-51.
    [10] Cocks LRM, Torsvik TH. Siberia, the wandering northern terrane, and its changing geography through the palaeozoic[J]. Earth-Science Reviews, 2007, 82:29-74.
    [11] Cocks LRM, Torsvik TH. Baltica from the late precambrian to mid-palaeozoic times:The gain and loss of a terrane's identity[J]. Earth-Science Reviews, 2005, 72:39-66.
    [12] Torsvik TH, Cocks LRM. Gondwana from top to base in space and time[J]. Gondwana Research, 2013, 24:999-1030.
    [13] 孙丽莎, 黄宝春. 塔里木地块奥陶纪古地磁新结果及其构造意义[J]. 地球物理学报, 2009, 52(7):1836-1848.

    [SUN Lisha,HUANG Baochun.New paleomagnetic results from Ordivician rocks from the Tarim blocks,nothwest China and its tectonic implications[J].Chinese Journal of Geophysics,2009,52(7):1836-1848.]
    [14] 景秀春, 邓胜徽, 王训练. 塔里木板块奥陶纪运动学特征:来自牙形石的证据[J]. 中国科技论文在线精品论文,2014,7(21):2113-2121.

    [JING Xiuchun,DENG Shenghui,WANG Xunlian.The kinematic characteristics of the Tarim paleoplate in the Ordovician:Evidence from conodonts[J].Highlights of Sciencepaper Online,2014,7(21):2113-2121.]
    [15] 侯方辉,张训华,温珍河,等.古生代以来中国主要块体活动古地理重建及演化[J].海洋地质与第四纪地质,2014,34(6):9-26.

    [HOU Fanghui,ZHANG Xunhua,WEN Zhenhe,et al.Paleogeographic reconstruction and tectonic evolution of major blocks in china since paleozoic[J].Marine Geology and Quaternary Geology,2014,34(6):9-26.]
    [16] Xiao W, Huang B, Han C, et al. A review of the western part of the altaids:A key to understanding the architecture of accretionary orogens[J]. Gondwana Research, 2010, 18:253-273.
    [17] 许志琴, 李思田, 张建新, 等. 塔里木地块与古亚洲/特提斯构造体系的对接[J]. 岩石学报, 2011, 27:1-22.[XU Zhiqin,LI Sitian,ZHANG Jianxin et al.Paleo-Asian and Tethyan tectonic systems with docking the Tarim plate[J].Acta Petrologica Sinica,2009

    ,27(1):1-22.]
    [18] 高俊, 钱青, 龙灵利, 等. 西天山的增生造山过程[J]. 地质通报, 2009, 28:1804-1816.[GAO Jun,QIAN Qing,LONG Lingli, et al.Accretionary orogenic process of West Tianshan[J].Geological Bulletin of China,2009

    ,28(12):1804-1816.]
    [19] 万天丰, 朱鸿. 古生代与三叠纪中国各陆块在全球古大陆再造中的位置与运动学特征[J]. 现代地质, 2007, 21(1):1-13.

    [Wan Tianfen,Zhu Hong.Positions and kinematics of Chinese continental blocks in restruction of Global paleo-continents for Paleozoic and Triassic[J].Geoscience,2007,27(1):1-13.]
    [20] Torsvik TH, Burke K, Steinberger B, et al. Diamonds sampled by plumes from the core-mantle boundary[J]. Nature, 2010, 466:352-355,Torsvik TH, Steinberger B, Gurnis M, et al. Plate tectonics and net lithosphere rotation over the past 150my[J]. Earth and Planetary Science Letters, 2010, 291:106-112.
    [21] Evans DAD. True polar wander and supercontinents[J]. Tectonophysics, 2003, 362:303-320.
    [22] Cocks LRM, Torsvik TH. The dynamic evolution of the palaeozoic geography of eastern asia[J]. Earth-Science Reviews, 2013, 117:40-79.
    [23] Hochard C, Stampfli G. Gis and Geodatabases Application to Global scale Plate Tectonics Modelling[M]. Lausanne,univ. of Lausanne,2008.
    [24] Gurnis M, Turner M, Zahirovic S, et al. Plate tectonic reconstructions with continuously closing plates[J]. Computers & Geosciences, 2012, 38:35-42.
    [25] Hartz EH, Torsvik TH. Baltica upside down:A new plate tectonic model for rodinia and the iapetus ocean[J]. Geology, 2002, 30:255-258.
    [26] van Staal CR, Whalen JB, Valverde-Vaquero P, et al. Pre-carboniferous, episodic accretion-related, orogenesis along the laurentian margin of the northern appalachians[J]. Geological Society, London, Special Publications, 2009, 327:271-316.
    [27] von Raumer JF, Stampfli GM. The birth of the rheic ocean-early palaeozoic subsidence patterns and subsequent tectonic plate scenarios[J]. Tectonophysics, 2008, 461:9-20.
    [28] Cawood PA. Terra australis orogen:Rodinia breakup and development of the pacific and iapetus margins of gondwana during the neoproterozoic and paleozoic[J]. Earth-Science Reviews, 2005, 69:249-279.
    [29] Dobretsov NL, Buslov MM, Vernikovsky VA. Neoproterozoic to early ordovician evolution of the paleo-asian ocean:Implications to the break-up of rodinia[J]. Gondwana Research, 2003, 6:143-159.
    [30] Li J-Y. Permian geodynamic setting of northeast china and adjacent regions:Closure of the paleo-asian ocean and subduction of the paleo-pacific plate[J]. Journal of Asian Earth Sciences, 2006, 26:207-224.
    [31] 王兴安. 华北板块北缘中段早古生代-泥盆纪构造演化[D]. 长春,吉林大学, 2014.[WANG Xingan.Tectonic evolution of the central segment of the northern margin of the north china plate from early paleozoic to devonian[D].Chang Chun,univ. of Jilin,2014.]
    [32] 黄宝春, 周姚秀, 朱日祥. 从古地磁研究看中国大陆形成与演化过程[J]. 地学前缘, 2008, 15(3):348-359.

    [HUANG Baochun,ZHOU Yaoxiu,ZHU Rixiang.Disscussions on the phanerozoic evolution and formation of continental China,based on paleomagnetic studies[J].Earth Science Frontier,2008,15(3):348-359.]
    [33] Bradley DC. Passive margins through earth history[J]. Earth-Science Reviews, 2008, 91:1-26.
    [34] 李三忠,余珊,赵淑娟,等.超大陆与全球板块重建派别[J].海洋地质与第四纪地质,2014,34(6):97-117.

    [LI Sanzhong,YU Shan,ZHAO Guochun,et al.Schools of thought on supercontinent and global plate reconstruction[J].Marine Geology and Quaternary Geology,2014,34(6):97-117.]
    [35] Meert JG, Van der Voo R, Powell CM, et al. A plate-tectonic speed limit?[J].Nature,1993,363:216-217.
  • [1] 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
    [2] 汪品先.  海洋地质与第四纪地质的结合 . 海洋地质与第四纪地质, 2021, 41(5): 1-2. doi: 10.16562/j.cnki.0256-1492.2021072601
    [3] 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:  873
  • HTML全文浏览量:  147
  • PDF下载量:  8
  • 被引次数: 0
出版历程
  • 收稿日期:  2014-12-11
  • 修回日期:  2015-01-29

奥陶纪到志留纪全球板块重建:中国三大陆块位置及其洋陆格局的运动学检验

doi: 10.16562/j.cnki.0256-1492.2015.04.019
    作者简介:

    聂仕琪(1989-),男,硕士,从事板块构造与地球动力学研究,Email:nsq@mail.ustc.edu.cn

基金项目:

国家自然科学基金项目(91014005,41474082)

国家自然科学基金重大项目(41190072)

  • 中图分类号: P736.1

摘要: 中国三大陆块是全球奥陶纪到志留纪板块与洋陆格局重建的关键,涉及到古亚洲洋与原特提斯洋的演化。综合了全球奥陶纪到志留纪的古地磁、古生物、古气候以及地球化学的相关证据,重建了中国三大陆块在这一时期的板块演化与洋陆格局,并将它们与全球板块演化模型结合到一起,特色在于通过板块运动的速度场分析,厘定了全球重要的板块边界及其性质。得到以下新认识:在奥陶纪到志留纪,中国三大陆块独立地位于地球的低纬地区,并且不依附于任何大的陆块,离散分布于原特提斯洋与古亚洲洋之间,原特提斯洋与古亚洲洋不断消减俯冲。其中,华北陆块早期靠近西伯利亚大陆东缘,华南陆块在奥陶纪早期沿着冈瓦纳大陆西侧漂移,塔里木陆块在奥陶纪进行了一个南北向的大范围的运动后,在志留纪开始向西漂移。中国三大陆块在这一时期不断地相互作用。在奥陶纪到中志留纪,原特提斯洋不断地俯冲冈瓦纳大陆与华北大陆,直到晚志留纪,随着古特提斯洋的扩张,原特提斯洋开始逐渐闭合。

English Abstract

参考文献 (35)

目录

    /

    返回文章
    返回