• 中国出版政府奖提名奖

    中国百强科技报刊

    湖北出版政府奖

    中国高校百佳科技期刊

    中国最美期刊

    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

    华夏早古生代俯冲作用(Ⅰ):来自糯垌蛇绿岩的新证据

    彭松柏 刘松峰 林木森 吴长峰 韩庆森

    彭松柏, 刘松峰, 林木森, 吴长峰, 韩庆森, 2016. 华夏早古生代俯冲作用(Ⅰ):来自糯垌蛇绿岩的新证据. 地球科学, 41(5): 765-778. doi: 10.3799/dqkx.2016.065
    引用本文: 彭松柏, 刘松峰, 林木森, 吴长峰, 韩庆森, 2016. 华夏早古生代俯冲作用(Ⅰ):来自糯垌蛇绿岩的新证据. 地球科学, 41(5): 765-778. doi: 10.3799/dqkx.2016.065
    Peng Songbai, Liu Songfeng, Lin Musen, Wu Changfeng, Han Qingsen, 2016. Early Paleozoic Subduction in Cathaysia (Ⅰ): New Evidence from Nuodong Ophiolite. Earth Science, 41(5): 765-778. doi: 10.3799/dqkx.2016.065
    Citation: Peng Songbai, Liu Songfeng, Lin Musen, Wu Changfeng, Han Qingsen, 2016. Early Paleozoic Subduction in Cathaysia (Ⅰ): New Evidence from Nuodong Ophiolite. Earth Science, 41(5): 765-778. doi: 10.3799/dqkx.2016.065

    华夏早古生代俯冲作用(Ⅰ):来自糯垌蛇绿岩的新证据

    doi: 10.3799/dqkx.2016.065
    基金项目: 

    中国地质调查局地质调查项目 12120114039201

    详细信息
      作者简介:

      彭松柏(1963-),男,教授,博士,主要从事岩石大地构造及蛇绿岩研究.E-mail:psongbai@aliyun.com

    • 中图分类号: P545

    Early Paleozoic Subduction in Cathaysia (Ⅰ): New Evidence from Nuodong Ophiolite

    • 摘要: 早古生代加里东期造山运动(广西运动)的性质是华南大地构造演化长期争议的重大地质问题.桂东南岑溪糯垌一带奥陶纪浅变质地层中出露一套变形变质基性岩系构造岩片,主要由变枕状玄武岩、辉绿岩墙以及少量块状辉长岩和辉石岩组成.变玄武岩、变辉绿岩的SiO2含量为49.20%~52.30%,MgO含量为6.78%~9.11%,Mg#为55~63,TiO2含量为1.02%~1.34%,属低钾拉斑玄武系列基性岩.稀土元素配分平坦,轻稀土亏损,(La/Sm)N为0.72~1.05,(La/Yb)N为0.7~1.0,无明显Eu异常,大离子亲石元素Rb、Ba、Th、U、K、Pb相对富集,高场强元素Nb、Ta、Zr、Hf、Ti平坦-略亏损,Ti/V为21.30~25.12,Nb/Th为2.1~4.2,表现出俯冲带之上(SSZ)蛇绿岩的地球化学特征.变辉绿岩LA-ICP-MS锆石U-Pb成岩年龄为437±5 Ma,表明其形成于早志留世.综合研究表明,糯垌变基性岩系应属早古生代形成于俯冲之上(SSZ)弧前构造环境的肢解蛇绿岩残片,这一发现为华南扬子克拉通与华夏地块之间存在早古生代洋盆和俯冲-增生碰撞造山提供了关键证据.

       

    • 图  1  华南大地构造基本单元(a)、糯垌地区地质简图(b)和糯垌变基性岩系地质剖面(c)

      图b据广西壮族自治区区域地质调查队1:5万地质图修编

      Fig.  1.  The tectonic framework of the South China (a), the geological sketch of Nuodong area (b) and geological section of the Nuodong metamorphic basic rock series (c)

      图  2  变玄武岩、辉绿岩及变辉石岩野外宏观和显微照片

      a.枕状玄武岩野外露头;b.杏仁状玄武岩野外露头;c.变辉绿岩岩脉(岩墙)群野外露头;d.强烈韧性剪切变形形成的玄武岩与辉绿岩岩脉(岩墙)似层状构造;e.变玄武岩中变余杏仁结构(正交镜);f.变辉绿岩中变余辉绿-辉长结构(单偏镜);g.变辉绿岩中变余辉绿结构(正交镜);h.变辉石岩中变余粒状结构(正交镜).矿物缩写:Prx.辉石;Hbl.角闪石;Pl.斜长石;Mag.磁铁矿;Q.石英

      Fig.  2.  Representative field and thin section photomicrographs of the metabasalt and metadiabase

      图  3  变玄武岩、辉绿岩岩石化学分类和岩浆岩系列判别

      a.Zr/Ti-Nb/Y岩石化学分类图(Floyd and Winchester, 1975; Pearce, 1996);b.Y-Zr岩浆系列判别图(Polat et al., 2009)

      Fig.  3.  Geochemical classification and magmatic series discriminant diagrams of the metabasalt and metadiabase

      图  4  变玄武岩、辉绿岩稀土元素球粒陨石标准化配分型式(a)和微量元素N-MORB标准化蛛网图(b)

      Fig.  4.  Chondrite-normalized REE diagram (a) and N-MORB-normalized trace elements spider-diagram of the metabasalt and metadiabase (b)

      图  5  变辉绿岩代表性锆石CL图像(a)及锆石年龄协和图(b)

      Fig.  5.  Representative CL images (a) and U-Pb concordia diagram for zircons of the metadiabase (b)

      图  6  变玄武岩、辉绿岩构造环境判别图

      a.2Nb-Zr/4-Y判别图解(Meschede, 1986);b.V-Ti判别图解(Shervais, 1982);c.Th/Yb-Ta/Yb判别图解(Pearce, 1982);d.Th/Yb-Nb/Yb判别图解(Pearce, 2008, 2014; Dilek and Furnes, 2011; Angerer et al., 2013).N-MORB.正常洋脊玄武岩;E-MORB.富集洋脊玄武岩;IAB.岛弧玄武岩;IAT.岛弧拉斑玄武岩;ICA.岛弧钙碱性玄武岩;CAB.钙碱性玄武岩;WPB.板内玄武岩;WPT.板内拉斑玄武岩;WPAB.板内碱性玄武岩;OIB.洋岛玄武岩;AB.弧玄武岩;SHO.钾玄岩;CFB.大陆溢流玄武岩;FAB.弧前玄武岩

      Fig.  6.  Tectonic discriminant diagrams of the metabasalt and diabase

      图  7  桂东南早古生代蛇绿岩和髙镁-镁质玄武岩-安山岩成因示意

      Fig.  7.  Genetic sketch of Early Paleozoic ophiolite and high magnesian-magnesian basalt-andesite in the southeastern Guangxi

      表  1  变玄武岩、辉绿岩主量元素(%)和微量元素(10-6)组成

      Table  1.   Major elements (%) and trace elements (10-6) composition of the metabasalt and metadiabase

      岩性 变玄武岩 变辉绿岩
      12ND03 14ND3-1 15ND1-1 12ND01 12ND02 12ND05 14ND1-1 14ND4-2
      SiO2 51.00 49.20 50.60 51.78 51.45 52.30 50.10 50.00
      TiO2 1.07 1.04 1.27 1.34 1.15 1.02 1.20 1.07
      Al2O3 15.04 15.10 15.00 14.87 14.43 15.63 14.50 15.20
      Fe2O3 2.41 2.24 2.57 2.61 2.75 1.98 2.49 1.84
      FeO 7.25 7.63 7.89 8.20 7.55 6.65 8.34 7.68
      MnO 0.18 0.19 0.17 0.16 0.17 0.13 0.18 0.18
      MgO 7.59 9.11 7.22 7.09 7.54 6.78 7.46 7.75
      CaO 10.63 11.70 9.48 8.07 10.21 11.30 10.15 12.10
      Na2O 3.01 2.20 3.19 4.15 2.53 2.17 2.80 2.48
      K2O 0.08 0.09 0.14 0.13 0.12 0.15 0.19 0.16
      P2O5 0.08 0.08 0.11 0.11 0.09 0.08 0.10 0.08
      LOI 0.88 0.69 0.61 0.90 1.21 1.00 0.52 0.63
      Total 99.22 99.27 98.25 99.33 99.20 99.19 98.03 99.17
      Mg# 59 63 56 55 58 59 56 60
      Ba 13.8 15.3 20.0 54.6 26.4 68.2 30.5 26.0
      Rb 1.3 0.7 1.7 0.9 2.7 3.4 2.7 1.9
      Th 0.54 0.61 0.82 0.74 0.96 0.90 0.80 0.59
      Pb 0.60 2.00 1.10 0.94 0.71 0.81 1.20 1.90
      Nb 2.11 2.10 3.10 2.57 2.67 1.93 3.30 2.30
      Sr 83.8 92.1 80.9 64.1 85.3 122.0 104.0 91.2
      Zr 57.4 60.0 69.0 74.7 69.1 62.8 72.0 60.0
      Y 28.0 26.4 34.5 36.0 33.3 28.4 34.4 26.7
      Cr 216 211 116 143 205 136 98 216
      V 301 282 303 370 303 273 303 283
      Ni 80.4 81.0 47.0 40.8 71.7 59.4 46.0 86.0
      Co 46.1 52.0 51.0 48.4 44.4 47.8 45.0 54.0
      Cs 0.08 0.06 0.18 0.08 0.16 0.24 0.20 0.02
      Ta 0.16 0.10 0.17 0.18 0.19 0.17 0.20 0.20
      Hf 1.70 1.90 2.10 2.28 2.05 1.84 2.20 1.90
      U 0.23 0.19 0.31 0.23 0.17 0.16 0.19 0.23
      La 2.73 3.00 4.30 3.81 4.11 3.28 4.40 3.20
      Ce 7.64 7.90 10.60 9.98 9.36 8.62 10.50 8.20
      Pr 1.24 1.31 1.68 1.65 1.69 1.38 1.70 1.33
      Nd 6.73 6.40 7.90 8.85 8.53 7.48 8.30 6.40
      Sm 2.46 2.29 2.92 3.05 2.82 2.55 2.70 2.21
      Eu 0.81 0.92 1.05 1.03 0.99 0.90 1.04 0.91
      Gd 3.42 3.46 4.71 4.40 4.00 3.41 4.11 3.45
      Tb 0.67 0.67 0.83 0.85 0.79 0.69 0.80 0.67
      Dy 4.62 4.54 5.41 5.93 5.44 4.66 5.48 4.26
      Ho 0.99 0.94 1.26 1.29 1.17 0.96 1.15 0.93
      Er 2.95 3.01 3.73 3.85 3.56 3.00 3.66 2.92
      Tm 0.41 0.44 0.62 0.57 0.51 0.43 0.50 0.41
      Yb 2.89 2.84 3.57 3.77 3.41 2.95 3.31 2.64
      Lu 0.44 0.40 0.55 0.57 0.53 0.45 0.48 0.40
      下载: 导出CSV

      表  2  变辉绿岩LA-ICP-MS锆石U-Pb测年结果

      Table  2.   Analyses results of LA-ICP-MS zircon U-Pb dating for the metadiabase

      测点 Th(10-6) U(10-6) Th/U同位素比值(±1σ) 年龄Ma(±1σ)
      207Pb/206Pb 207Pb/235U 206Pb/238U 207Pb/206Pb 207Pb/235U 206Pb/238U
      1 1 129 963 1.17 0.054 5±0.001 3 0.538 6±0.012 9 0.071 2±0.000 7 391±49.1 437±8.5 443±4.1
      2 127 167 0.76 0.069 1±0.002 4 1.141 8±0.040 5 0.119 1±0.001 5 902±72.2 773±19.2 725±8.4
      3 1 245 1 879 0.66 0.056 1±0.001 3 0.541 4±0.012 1 0.069 4±0.000 6 457±50.0 439±8.0 433±3.9
      4 466 550 0.85 0.056 2±0.001 9 0.566 0±0.018 6 0.072 5±0.000 8 461±106 455±12.1 451±4.5
      5 214 386 0.55 0.054 5±0.002 0 0.545 2±0.019 9 0.072 0±0.000 8 391±81.5 442±13.1 448±5.0
      6 186 294 0.63 0.056 6±0.002 5 0.535 6±0.023 6 0.068 3±0.000 9 476±98.1 435±15.6 426±5.4
      7 395 778 0.51 0.056 4±0.001 7 0.563 2±0.015 8 0.072 0±0.000 6 478±32.4 454±10.3 448±3.8
      8 426 465 0.92 0.055 7±0.001 7 0.544 1±0.017 4 0.069 9±0.000 7 443±68.5 441±11.4 435±4.1
      9 742 1178 0.63 0.055 1±0.001 4 0.524 5±0.013 4 0.068 3±0.000 6 417±54.6 428±8.9 426±3.8
      10 535 672 0.80 0.055 2±0.001 8 0.535 3±0.016 8 0.069 7±0.000 8 420±76.8 435±11.1 434±4.5
      11 116 666 0.17 0.121 0±0.003 0 5.825 3±0.137 6 0.345 4±0.003 1 1 972±43.8 1 950±20.5 1 912±14.9
      12 333 711 0.47 0.054 9±0.001 6 0.535 7±0.015 7 0.070 1±0.000 7 409±66.7 436±10.4 437±4.2
      13 497 523 0.95 0.055 8±0.002 0 0.529 8±0.018 1 0.068 4±0.000 8 443±79.6 432±12.0 427±4.6
      14 351 467 0.75 0.064 3±0.002 1 0.996 7±0.043 4 0.109 1±0.002 9 750±69.3 702±22.1 668±16.8
      15 299 618 0.48 0.053 6±0.002 1 0.532 2±0.021 7 0.071 4±0.000 9 354±90.7 433±14.4 445±5.5
      16 828 838 0.99 0.053 9±0.001 9 0.532 6±0.017 7 0.071 4±0.000 8 369±84.3 434±11.7 444±4.8
      17 315 469 0.67 0.052 7±0.001 8 0.580 9±0.019 4 0.079 3±0.001 0 317±75.9 465±12.4 492±5.8
      18 285 461 0.62 0.106 5±0.002 6 4.444 6±0.107 5 0.299 8±0.002 9 1 740±44.8 1 721±20.1 1 690±14.5
      19 1 167 1 016 1.15 0.055 6±0.001 5 0.538 0±0.014 0 0.069 6±0.000 7 435±59.3 437±9.3 434±4.2
      20 371 647 0.57 0.056 0±0.001 8 0.533 9±0.016 8 0.068 9±0.000 6 454±67.6 434±11.1 429±3.8
      下载: 导出CSV
    • Angerer, T., Kerrich, R., Hagemann, S.G., 2013.Geochemistry of a Komatiitic, Boninitic, and Tholeiitic Basalt Association in the Mesoarchean Koolyanobbing Greenstone Belt, Southern Cross Domain, Yilgarn Craton:Implications for Mantle Sources and Geodynamic Setting of Banded Iron Formation.Precambrian Research, 224:110-128.doi: 10.1016/j.precamres.2012.09.012
      Cawood, P.A., Wang, Y., Xu, Y., et al., 2013.Locating South China in Rodinia and Gondwana:A Fragment of Greater India Lithosphere? Geology, 41(8):903-906.doi: 10.1130/g34395.1
      Charvet, J., 2013.The Neoproterozoic-Early Paleozoic Tectonic Evolution of the South China Block:An Overview.Journal of Asian Earth Sciences, 74:198-209.doi: 10.1016/j.jseaes.2013.02.015
      Charvet, J., Shu, L.S., Faure, M., et al., 2010.Structural Development of the Lower Paleozoic Belt of South China:Genesis of an Intracontinental Orogen.Journal of Asian Earth Sciences, 39(4):309-330.doi: 10.1016/j.jseaes.2010.03.006
      Chen, H.D., Hou, M.C., Xu, X.S., et al., 2006.Tectonic Evolution and Sequence Stratigraphic Framework in South China during Caledonian.Journal of Chengdu University of Technology (Science & Technology Edition), 33(1):1-8(in Chinese with English abstract). https://www.researchgate.net/publication/283809291_Tectonic_evolution_and_sequence_stratigraphic_framework_in_South_China_during_Caledonian
      Chen, X., Zhang, Y.D., Fan, J.X., et al., 2012.Onset of the Kwangsian Orogeny as Evidenced by Biofacies and Lithofacies.Science China:Earth Sciences, 42(11):1617-1626(in Chinese). http://www.cnki.com.cn/Article/CJFDTotal-JDXG201210004.htm
      Chen, X.Y., Tong, L.X., Zhang, C.L., et al., 2015.Retrograde Garnet Amphibolite from Eclogite of the Zhejiang Longyou Area:New Evidence of the Caledonian Orogenic Event in the Cathaysia Block.Chinese Science Bulletin, 60(13):1207-1217 (in Chinese). doi: 10.1360/N972015-00094
      Dilek, Y., Furnes, H., 2011.Ophiolite Genesis and Global Tectonics:Geochemical and Tectonic Fingerprinting of Ancient Oceanic Lithosphere.Geological Society of America Bulletin, 123(3-4):387-411.doi: 10.1130/b30446.1
      Dilek, Y., Furnes, H., 2014.Ophiolites and Their Origins.Elements, 10(2):93-100.doi: 10.2113/gselements.10.2.93
      Du, Y.S., Xu, Y.J., 2012.A Preliminary Study on Caledonian Event in South China.Geological Science and Technology Information, 31(5):43-49 (in Chinese with English abstract). https://www.researchgate.net/publication/309373333_A_Preliminary_Study_on_Caledonian_Event_in_South_China
      Faure, M., Shu, L.S., Wang, B., et al., 2009.Intracontinental Subduction:A Possible Mechanism for the Early Palaeozoic Orogen of SE China.Terra Nova, 21(5):360-368.doi: 10.1111/j.1365-3121.2009.00888.x
      Floyd, P.A., Winchester, J.A., 1975.Magma Type and Tectonic Setting Discrimination Using Immobile Elements.Earth and Planetary Science Letters, 27(2):211-218.doi: 10.1016/0012-821x(75)90031-x
      Guo, L.Z., Shi, Y.S., Lu, H.F., et al., 1989.The Pre-Devonian Tectonic Patterns and Evolution of South China.Journal of Southeast Asian Earth Sciences, 3(1-4):87-93.doi: 10.1016/0743-9547(89)90012-3
      He, W.H., Zhang, K.X., Wu, S.B., et al., 2015.End-Permian Faunas from Yangtze Basin and Its Marginal Region:Implications for Palaeogeographical and Tectonic Environments.Earth Science, 40(2):275-289 (in Chinese with English abstract). https://www.researchgate.net/publication/282196826_End-permian_faunas_from_Yangtze_basin_and_its_marginal_region_Implications_for_palaeogeographical_and_tectonic_environments
      Hsü, K.J., Li, J.L., Chen, H.H., et al., 1990.Tectonics of South China:Key to Understanding West Pacific Geology.Tectonophysics, 183(1-4):9-39.doi: 10.1016/0040-1951(90)90186-c
      Li, J.L., 2004.Basic Characteristics of Accretion-Type Orogens.Geological Bulletin of China, 23(9-10):947-951 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD2004Z2017.htm
      Li, J.L., 2009.Global Tectonic Fades:A Preclusive Opinion.Geological Bulletin of China, 28(10):1375-138l (in Chinese with English abstract).s https://www.researchgate.net/publication/289256202_Global_tectonic_facies_A_preclusive_opinion
      Li, Y.J., Kuang, G.D., Wu, H.R., et al., 1993.Qinzhou Foreland Basin—New Understandings about the Qinzhou Residual Trough.Guangxi Geology, 6(4):13-18 (in Chinese with English abstract).
      Li, Z.X., 1998.Tectonic History of the Major East Asian Lithospheric Blocks since the Mid-Proterozoic:A Synthesis.Geodynamics Series, 221-243.doi: 10.1029/gd027p0221
      Li, Z.X., Li, X.H., Wartho, J.A., et al., 2010.Magmatic and Metamorphic Events during the Early Paleozoic Wuyi-Yunkai Orogeny, Southeastern South China:New Age Constraints and Pressure-Temperature Conditions.Geological Society of America Bulletin, 122(5-6):772-793.doi: 10.1130/B30021.1
      Lin, M.S., Peng, S.B., Jiang, X.F., et al., 2015.Geochemistry, Petrogenesis and Tectonic Setting of Neoproterozoic Mafic-Ultramafic Rocks from the Western Jiangnan Orogen, South China.Gondwana Research.[2016-06-19]http://dx.doi.org/10.1016/j.gr.2015.05.015
      Lin, W., Faure, M., Lepvrier, C., et al., 2011.The Early Mesozoic Thrust and Folds Sheet Structure along the Southern Margin of South China Block and Its Geodynamic.Chinese Journal of Geology, 46(1):134-145 (in Chinese with English abstract). https://www.researchgate.net/publication/286794869_The_Early_Mesozoic_thrust_and_folds_sheet_structure_along_the_southern_margin_of_South_China_Block_and_its_geodynamic
      Liu, B.J., Xu, X.S., Pan, X.N., et al., 1993.Paleocontinental Sediments, Crust Evolution and Ore Deposits of South China.Science Press, Beijing, 120-134(in Chinese).
      Liu, Y.L., Zhou, X.J., Liao, Z.T., et al., 2009.Relative Blocks and Convergence Process during the Caledonian Movement in South China.Petroleum Geology & Experiment, 31(1):19-25(in Chinese with English abstract).
      Liu, Y.S., Hu, Z.C., Gao, S., et al., 2008.In Situ Analysis of Major and Trace Elements of Anhydrous Minerals by LA-ICP-MS without Applying an Internal Standard.Chemical Geology, 257:34-43. doi: 10.1016/j.chemgeo.2008.08.004
      Liu, Y.S., Hu, Z.C., Zong, K.Q., et al., 2010.Reappraisement and Refinement of Zircon U-Pb Isotope and Trace Element Analyses by LA-ICP-MS.Chinese Science Bulletin, 55(15):1535-1546.doi: 10.1007/s11434-010-0052-3
      Lu, J.P., Kang, Y.J., 1999.Geological Feature of Devonian and Silurian System in Cenxi Guangxi and Its Significance.Guangxi Geology, 12(1):9-14(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GXDZ901.001.htm
      Lu, Y.F., 2004.GeoKit:A Geochemical Toolkit for Microsoft Excel.Geochimica, 33(5):459-464 (in Chinese with English abstract).
      Ludden, J., Gélinas, L., Trudel, P., 1982.Archean Metavolcanics from the Rouyn-Noranda District, Abitibi Greenstone Belt, Quebec.2.Mobility of Trace Elements and Petrogenetic Constraints.Canadian Journal of Earth Sciences, 19(12):2276-2287.doi: 10.1139/e82-200
      Ludwing, K.R., 2003.Users Manual for Isoplot 3.0:A Geochronological Toolkit for Microsoft Excel.Berkeley Geochronology Center, Berkeley, 35:1-39.
      Ma, R.S., 2006.New Thought about the Tectonic Evolution of the South China:With Discussion on Several Problems of the Cathaysian Old Land.Geological Journal of China Universities, 12(4):448-456(in Chinese with English abstract). https://www.researchgate.net/publication/284544644_New_thought_about_the_tectonic_evolution_of_South_China_with_discussion_on_several_problems_of_the_Cathaysian_old_land
      Meschede, M., 1986.A Method of Discriminating between Different Types of Mid-Ocean Ridge Basalts and Contienetal Tholeiites with Nd-Zr-Y Diagram.Chemical Geology, 56(3-4):207-218.doi: 10.1016/0009-2541(86)90004-5
      Murphy, J.B., Hynes, A.J., 1986.Contrasting Secondary Mobility of Ti, P, Zr, Nb, and Y in Two Metabasaltic Suites in the Appalachians.Canadian Journal of Earth Sciences, 23(8):1138-1144.doi: 10.1139/e86-112
      Pan, G.T., Xiao, Q.H., Lu, S.N., et al., 2008.Definition, Classification, Characteristics and Diagnostic Indications of Tectonic Facies.Geological Bulletin of China, 27(10):1613-1637(in Chinese with English abstract). https://www.researchgate.net/publication/285732732_Definition_classification_characteristics_and_diagnostic_indications_of_tectonic_facies
      Pearce, J.A., 2008.Geochemical Fingerprinting of Oceanic Basalts with Applications to Ophiolite Classification and the Search for Archean Oceanic Crust.Lithos, 100(1-4):14-48.doi: 10.1016/j.lithos.2007.06.016
      Pearce, J.A., 2014.Immobile Element Fingerprinting of Ophiolites.Elements, 10(2):101-108.doi: 10.2113/gselements.10.2.101
      Pearce, J.A., Lippard, S.J., Roberts, S., 1984.Characteristics and Tectonic Significance of Supra-Subduction Zone Ophiolites.Geological Society, London, Special Publications, 16(1):77-94.doi: 10.1144/gsl.sp.1984.016.01.06
      Pearce, J.A., 1982.Trace Element Characteristics of Lavas from Destructive Plate Boundaries.In:Thorpe, R.S., ed., Orogenic Andesites and Related Rocks.John Wiley and Sons, Chichester, 528-548.
      Pearce, J.A., 1996.A User's Guide to Basalt Discrimination Diagrams.In:Wyman, D.A.ed., Trace Elements Geochemistry of Volcanic Rocks:Applications for Massive Sulphide Exploration.Geological Association of Canada, Newfoundland, 79-113.
      Peng, S.B., Jin, Z.M., Fu, J.M., et al., 2006.The Petrochemistry, Chronology and Tectonic Setting of Strong Peraluminous Anatectic Granitoids in Yunkai Orogenic Belt, Western Guangdong Province, China.Earth Science, 31(1):110-120 (in Chinese with English abstract). https://www.researchgate.net/publication/248577798_Petrochemistry_Chronology_and_Tectonic_Setting_of_Strong_Peraluminous_Anatectic_Granitoids_in_Yunkai_Orogenic_Belt_Western_Guangdong_Province_China
      Polat, A., Hofmann, A.W., 2003.Alteration and Geochemical Patterns in the 3.7-3.8 Ga Isua Greenstone Belt, West Greenland.Precambrian Research, 126(3-4):197-218.doi: 10.1016/s0301-9268(03)00095-0
      Polat, A., Ross, P.S., Bédard, J.H., 2009.Magmatic Affinity of Modern and Ancient Subalkaline Volcanic Rocks Determined from Trace-Element Discriminant Diagrams.Canadian Journal of Earth Sciences, 46(11):823-839.doi: 10.1139/e09-054
      Qin, X.F., Wang, Z.Q., Hu, G.A., et al., 2013.Geochronology and Geochemistry of Hudong Gneissic Composite Pluton in the Junction of Guangdong and Guangxi Provinces:Implications for Early Paleozoic Tectono-Magmatism along the Northern Margin of Yunkai Massif.Acta Petrologica Sinica, 29(9):3115-3130(in Chinese with English abstract). https://www.researchgate.net/publication/295605443_Geochronology_and_geochemistry_of_Hudong_gneissic_composite_pluton_in_the_junction_of_Guangdong_and_Guangxi_provinces_Implications_for_Early_Paleozoic_tectono-magmatism_along_the_northern_margin_of_Yu
      Qin, X.F., Wang, Z.Q., Wang, T., et al., 2015.The Reconfirmation of Age and Tectonic Setting of the Volcanic Rocks of Yingyangguan Group in the Eastern Guangxi:Constraints on the Structural Pattern of the Southwestern Segment of Qinzhou-Hangzhou Joint Belt.Acta Geoscientica Sinica, 36(3):283-292(in Chinese with English abstract). https://www.researchgate.net/publication/282071585_The_reconfirmation_of_age_and_tectonic_setting_of_the_volcanic_rocks_of_Yingyangguan_group_in_the_eastern_Guangxi_Constraints_on_the_structural_pattern_of_the_southwestern_segment_of_Qinzhou-Hangzhou_
      Qiu, Y.X., Liang, X.Q., 2006.Evolution of Basin-Range Coupling in the Yunkai Dashan-Shiwan Dashan Area, Guangdong and Guangxi:With a Discussion of Several Tectonic Problems of South China.Geological Bulletin of China, 25(3):340-347(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD200603004.htm
      Shervais, J.W., 1982.Ti-V Plots and the Petrogenesis of Modern and Ophiolitic Lavas.Earth and Planetary Science Letters, 59(1):101-118.doi: 10.1016/0012-821x(82)90120-0
      Shi, R.D., 2005.Comment on the Progress in and Problems on Ophiolite Study.Geological Review, 51(6):681-693 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP200506013.htm
      Shu, L.S., 2006.Predevonian Tectonic Evolution of South China:From Cathaysian Block to Caledonian Period Folded Orogenic Belt.Geological Journal of China Universities, 12(4):418-431 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GXDX200604002.htm
      Shu, L.S., 2012.An Analysis of Principal Features of Tectonic Evolution in South China Block.Geological Bulletin of China, 31(7):1035-1053 (in Chinese with English abstract). https://www.researchgate.net/publication/279561053_An_analysis_of_principal_features_of_tectonic_evolution_in_South_China_Block
      Su, W.B., Huff, W.D., Ettensohn, F.R., et al., 2009.K-Bentonite, Black-Shale and Flysch Successions at the Ordovician-Silurian Transition, South China:Possible Sedimentary Responses to the Accretion of Cathaysia to the Yangtze Block and Its Implications for the Evolution of Gondwana.Gondwana Research, 15(1):111-130.doi: 10.1016/j.gr.2008.06.004
      Sun, S.S., McDonough, W.F., 1989.Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes.Geological Society, London, Special Publications, 42(1):313-345.doi: 10.1144/gsl.sp.1989.042.01.19
      Wang, J., Li, Z.X., 2003.History of Neoproterozoic Rift Basins in South China:Implications for Rodinia Break-Up.Precambrian Research, 122(1-4):141-158.doi: 10.1016/s0301-9268(02)00209-7
      Wang, Y.J., Fan, W.M., Zhao, G.C., et al., 2007.Zircon U-Pb Geochronology of Gneissic Rocks in the Yunkai Massif and Its Implications on the Caledonian Event in the South China Block.Gondwana Research, 12(4):404-416.doi: 10.1016/j.gr.2006.10.003
      Wu, H.R., 2000.A Discussion on the Tectonic Palaeogeography Related to the Caledonian Movement in Guangxi.Journal of Palaeogeography, 2(1):70-76 (in Chinese with English abstract). https://www.researchgate.net/publication/285745173_A_discussion_on_the_tectonic_Palaeogeography_related_to_the_Caledonian_movement_in_Guanxi
      Wu, H.R., 2005.Discussion on Tectonopalaeogeography of Lower Yangtze Area during the Caledonian Period.Journal of Palaeogeography, 7(2):243-248(in Chinese with English abstract).
      Xu, X.S., Liu, W., Men, Y.P., et al., 2012.Probe into the Tectonic Nature of Neoproterozoic Southern Hunan-Northern Guangxi Marine Basin.Acta Geologica Sinica, 86(12):1890-1904 (in Chinese with English abstract). https://www.researchgate.net/publication/312371825_Probe_into_the_Tectonic_Nature_of_Neoproterozoic_Southern_Hunan-Northern_Guangxi_Marine_Basin
      Yi, L.W., Ma, C.Q., Wang, L.X., et al., 2014.Discovery of Late Ordovician Subvolcanic Rocks in South China:Existence of Subduction-Related Dacite from Early Paleozoic? Earth Science, 39(6):637-653 (in Chinese with English abstract). https://www.researchgate.net/publication/286484139_Discovery_of_Late_Ordovician_subvolcanic_rocks_in_South_China_existence_of_subduction-related_dacite_from_Early_Paleozoic
      Yin, F.G., Xu, X.S., Wan, F., et al., 2001.The Sedimentary Response to the Evolutionary Process of Caledonian Foreland Basin System in South China.Acta Geoscientia Sinica, 22(5):425-428 (in Chinese with English abstract). https://www.researchgate.net/publication/281366839_The_sedimentary_response_to_the_evolutionary_process_of_Caledonian_foreland_basin_system_in_South_China
      Yin, H.F., Wu, S.B., Du, Y.S., et al., 1999.South China Defined as Part of Tethyan Archipelagic Ocean System.Earth Science, 24(1):1-12 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX901.000.htm
      Yu, J.H., Lou, F.S., Wang, L.J., et al., 2014.The Geological Significance of a Paleozoic Mafic Granulite Found in the Yiyang Area of Northeastern Jiangxi Province.Chinese Science Bulletin, 59(35):3508-3516(in Chinese). doi: 10.1360/N972014-00395
      Zhang, C.L., Santosh, M., Zhu, Q.B., et al., 2015.The Gondwana Connection of South China:Evidence from Monazite and Zircon Geochronology in the Cathaysia Block.Gondwana Research, 28(3):1137-1151.doi: 10.1016/j.gr.2014.09.007
      Zhang, F.R., Shu, L.S., Wang, D.Z., et al., 2009.Discussions on the Tectonic Setting of Caledonian Granitoids in the Eastern Segment of South China.Earth Science Frontiers, 16(1):248-260 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY200901034.htm
      Zhang, G.W., Guo, A.L., Wang, Y.J., et al., 2013.Tectonics of South China Continent and Its Implications.Science China:Earth Sciences, 43(10):1553-1582 (in Chinese). https://www.researchgate.net/publication/264116293_Tectonics_of_South_China_Continent_and_its_implications
      Zhang, J., Deng, J.F., Xiao, Q.H., et al., 2012.New Advances in the Study of Ophiolites.Geological Bulletin of China, 31(1):1-12(in Chinese with English abstract). https://www.researchgate.net/publication/285849808_New_advances_in_the_study_of_ophiolites
      Zhang, Q., Zhou, G.Q., 2001.Ophiolites in China.Science Press, Beijing (in Chinese).
      Zhao, G.C., Cawood, P.A., 2012.Precambrian Geology of China.Precambrian Research, 222-223:13-54.doi: 10.1016/j.precamres.2012.09.017
      陈洪德, 侯明才, 许效松, 等, 2006.加里东期华南的盆地演化与层序格架.成都理工大学学报(自然科学版), 33(1):1-8. http://www.cnki.com.cn/Article/CJFDTOTAL-CDLG200601000.htm
      陈相艳, 仝来喜, 张传林, 等, 2015.浙江龙游石榴石角闪岩(退变榴辉岩):华夏加里东期碰撞造山事件的新证据.科学通报, 60(13):1207-1217. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB201513008.htm
      陈旭, 张元动, 樊隽轩, 等, 2012.广西运动的进程:来自生物相和岩相带的证据.中国科学:地球科学, 42(11):1617-1626. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201211002.htm
      杜远生, 徐亚军, 2012.华南加里东运动初探.地质科技情报.31 (5):43-49. http://www.cnki.com.cn/Article/CJFDTOTAL-KJTB201211012.htm
      何卫红, 张克信, 吴顺宝, 等, 2015.二叠纪末扬子海盆及其周缘动物群的特征和古地理、古构造启示.地球科学, 40(2):275-289. http://www.earth-science.net/WebPage/Article.aspx?id=3046
      李继亮, 2004.增生型造山带的基本特征.地质通报, 23(9-10):947-951. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD2004Z2017.htm
      李继亮, 2009.全球大地构造相刍议.地质通报, 28(10):1375-1381. doi: 10.3969/j.issn.1671-2552.2009.10.002
      李曰俊, 邝国敦, 吴浩若, 等, 1993.钦州前陆盆地-关于钦州残余海槽的新认识.广西地质, 6(4):13-18. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDZ199304001.htm
      林伟, Faure, M., Lepvrier, C., 等, 2011.华南板块南缘早中生代的逆冲推覆构造及其相关的动力学背景.地质科学, 46(1):134-145. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX201101012.htm
      刘宝珺, 许效松, 潘杏南, 等, 1993.中国南方古大陆沉积地壳演化与成矿.北京:科学出版社, 120-134.
      刘运黎, 周小进, 廖宗庭, 等, 2009.华南加里东期相关地块及其汇聚过程探讨.石油实验地质, 31(1):19-25. doi: 10.11781/sysydz200901019
      陆济璞, 康云骥, 1999.广西岑溪地区泥盆系志留系地质特征及其意义.广西地质, 12(1):9-14. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDZ901.001.htm
      路远发, 2004.GeoKit:一个用VBA构建的地球化学工具软件包.地球化学, 33(5):459-464. http://www.cnki.com.cn/Article/CJFDTOTAL-DQHX200405003.htm
      马瑞士, 2006.华南构造演化新思考——兼论"华夏古陆"说中的几个问题.高校地质学报, 12(4):448-456. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX200604005.htm
      潘桂棠, 肖庆辉, 陆松年, 等, 2008.大地构造相的定义、划分、特征及其鉴别标志.地质通报, 27(10):1613-1637. doi: 10.3969/j.issn.1671-2552.2008.10.004
      彭松柏, 金振民, 付建明, 等, 2006, 云开造山带强过铝深熔花岗岩地球化学、年代学及构造背景.地球科学, 31(1):110-120. http://www.earth-science.net/WebPage/Article.aspx?id=1543
      覃小锋, 王宗起, 胡贵昂, 等, 2013.两广交界地区壶垌片麻状复式岩体的年代学和地球化学:对云开地块北缘早古生代构造-岩浆作用的启示.岩石学报, 29(9):3115-3130. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201309013.htm
      覃小锋, 王宗起, 王涛, 等, 2015.桂东鹰扬关群火山岩时代和构造环境的重新厘定:对钦杭结合带西南段构造格局的制约.地球学报, 36(3):283-292. doi: 10.3975/cagsb.2015.03.03
      丘元禧, 梁新权, 2006.两广云开大山—十万大山地区盆山耦合构造演化——兼论华南若干区域构造问题.地质通报, 25(3):340-347. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200603004.htm
      史仁灯, 2005.蛇绿岩研究进展、存在问题及思考.地质论评, 51(6):681-693. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP200506013.htm
      舒良树, 2006.华南前泥盆纪构造演化:从华夏地块到加里东期造山带.高校地质学报, 12(4):418-431. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX200604002.htm
      舒良树, 2012.华南构造演化的基本特征.地质通报, 31(7):1035-1053. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201207004.htm
      吴浩若, 2000.广西加里东运动构造古地理问题.古地理学报, 2(1):70-76. http://www.cnki.com.cn/Article/CJFDTOTAL-GDLX200001008.htm
      吴浩若, 2005.下扬子区加里东期构造古地理问题.古地理学报, 7(2):243-248. http://www.cnki.com.cn/Article/CJFDTOTAL-GDLX200502010.htm
      许效松, 刘伟, 门玉澎, 等, 2012.对新元古代湘桂海盆及邻区构造属性的探讨.地质学报, 86(12):1890-1904. doi: 10.3969/j.issn.0001-5717.2012.12.003
      易立文, 马昌前, 王连训, 等, 2014.华南晚奥陶世次火山岩的发现:早古生代与俯冲有关的英安岩?地球科学, 39(6):637-653. http://www.earth-science.net/WebPage/Article.aspx?id=2872
      尹福光, 许效松, 万方, 等, 2001.华南地区加里东期前陆盆地演化过程中的沉积响应.地球学报, 22(5):425-428. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXB200105008.htm
      殷鸿福, 吴顺宝, 杜远生, 等, 1999.华南是特提斯多岛洋体系的一部分.地球科学, 24(1):1-12. http://www.earth-science.net/WebPage/Article.aspx?id=749
      于津海, 楼法生, 王丽娟, 等, 2014.赣东北弋阳早古生代麻粒岩的发现及其地质意义.科学通报, 59(35):3508-3516. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB201435010.htm
      张芳荣, 舒良树, 王德滋, 等, 2009.华南东段加里东期花岗岩类形成构造背景探讨.地学前缘, 16(1):248-260. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200901034.htm
      张国伟, 郭安林, 王岳军, 等, 2013.中国华南大陆构造与问题.中国科学:地球科学.43(10):1553-1582. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201310003.htm
      张进, 邓晋福, 肖庆辉, 等, 2012.蛇绿岩研究的最新进展.地质通报, 31(1):1-12. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201201000.htm
      张旗, 周国庆, 2001.中国蛇绿岩.北京:科学出版社.
    • 加载中
    图(7) / 表(2)
    计量
    • 文章访问数:  6445
    • HTML全文浏览量:  2598
    • PDF下载量:  60
    • 被引次数: 0
    出版历程
    • 收稿日期:  2016-01-16
    • 刊出日期:  2016-05-15

    目录

      /

      返回文章
      返回