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    东昆仑中泥盆世A型花岗岩的确定及其构造意义

    刘彬 马昌前 郭盼 张金阳 熊富浩 黄坚 蒋红安

    刘彬, 马昌前, 郭盼, 张金阳, 熊富浩, 黄坚, 蒋红安, 2013. 东昆仑中泥盆世A型花岗岩的确定及其构造意义. 地球科学, 38(5): 947-962. doi: 10.3799/dqkx.2013.093
    引用本文: 刘彬, 马昌前, 郭盼, 张金阳, 熊富浩, 黄坚, 蒋红安, 2013. 东昆仑中泥盆世A型花岗岩的确定及其构造意义. 地球科学, 38(5): 947-962. doi: 10.3799/dqkx.2013.093
    LIU Bin, MA Chang-qian, GUO Pan, ZHANG Jin-yang, XIONG Fu-hao, HUANG Jian, JIANG Hong-an, 2013. Discovery of the Middle Devonian A-type Granite from the Eastern Kunlun Orogen and Its Tectonic Implications. Earth Science, 38(5): 947-962. doi: 10.3799/dqkx.2013.093
    Citation: LIU Bin, MA Chang-qian, GUO Pan, ZHANG Jin-yang, XIONG Fu-hao, HUANG Jian, JIANG Hong-an, 2013. Discovery of the Middle Devonian A-type Granite from the Eastern Kunlun Orogen and Its Tectonic Implications. Earth Science, 38(5): 947-962. doi: 10.3799/dqkx.2013.093

    东昆仑中泥盆世A型花岗岩的确定及其构造意义

    doi: 10.3799/dqkx.2013.093
    基金项目: 

    国家自然科学基金项目 41272079

    中国地质调查局计划项目 1212011121270

    中国地质调查局计划项目 1212010918002

    教育部和国家外国专家局高等学校学科创新引智计划 B07039

    详细信息
      作者简介:

      刘彬(1987-), 男, 博士研究生, 矿物学、岩石学、矿床学专业.E-mail: liubincug@126.com

      通讯作者:

      马昌前, E-mail: cqma@cug.edu.cn

    • 中图分类号: P581

    Discovery of the Middle Devonian A-type Granite from the Eastern Kunlun Orogen and Its Tectonic Implications

    • 摘要: 东昆仑中泥盆世冰沟正长花岗岩具有高硅(SiO2含量为71.85%~72.77%)和高碱(K2O+Na2O值为8.39~8.58)、相对富铝(A/CNK为0.93~1.03)、高FeOt/MgO(6.24~7.86)和104 Ga/Al值(3.04~3.60)、富集轻稀土、明显的Eu负异常、相对原始地幔明显富集Zr、Ga、Y和Hf等高场强元素并强烈亏损Ba、Sr、P和Ti元素的特征, 这些特征与A型花岗岩类的地球化学特征一致.采用锆石LA-ICP-MS U-Pb法获得206Pb/238U值加权平均年龄为391±3 Ma(MSWD值为2.36), 表明该岩体为中泥盆世岩浆活动的产物.综合全岩Sr-Nd同位素、地球化学及实验岩石学等资料, 可以判断该岩石为造山后伸展阶段长英质地壳物质(变杂砂岩)在低压高温氧化条件下发生部分熔融的产物.冰沟正长花岗岩是目前东昆仑地区报道的时代最晚的古生代A型花岗岩, 它的出现可能标志着中泥盆世时期东昆仑始特提斯构造演化的彻底终结和古特提斯构造演化的崭新开始.

       

    • 图  1  东昆仑造山带东段大地构造位置(a)和侵入岩地质分布(b)

      Fig.  1.  The tectonic location (a) and simplified geological map (b) of east part of the eastern Kunlun orogen

      图  2  冰沟正长花岗岩岩体地质简图

      1.奥陶纪花岗岩;2.中泥盆世正长花岗岩;3.中三叠世花岗岩;4.古元古代地层;5.中元古代地层;6.第四纪;7.采样位置;8.样品号

      Fig.  2.  Simplified geological map of the Binggou syeno-granitic pluton

      图  3  冰沟正长花岗岩显微镜下照片

      a.条纹结构;b.蠕虫结构;Bt.黑云母;Kfs.碱性长石;Pl.斜长石;Qtz.石英

      Fig.  3.  Photomicrographs of the typical textures of the Binggou syeno-granite

      图  4  冰沟正长花岗岩样品(09NM14-1)典型锆石阴极发光图像(a)和U-Pb谐和图(b)

      Fig.  4.  CL images of representative zircons from the Binggou syeno-granite (a) and the U-Pb zircon concordia diagram (b)

      图  5  冰沟正长花岗岩FeOt/(FeOt+MgO)-SiO2(a),(Na2O+K2O-CaO)-SiO2(b),FeOt/(FeOt+MgO)-Al2O3(c)和FeOt/(FeOt+MgO)-Al2O3/(K2O/Na2O)(d)图解(其中图a和b底图据Frost et al., 2001,图c和图d底图据Dall'Agnol and de Oliveira, 2007)

      Fig.  5.  FeOt/(FeOt+MgO) vs.SiO2 (a), (Na2O+K2O-CaO) vs.SiO2 (b), FeOt/(FeOt+MgO) vs.Al2O3 (c) and FeOt/(FeOt+MgO) vs.Al2O3/(K2O/Na2O) (d)plots for the Binggou syeno-granite

      图  6  冰沟正长花岗岩稀土元素球粒陨石标准化分布型式(a)(球粒陨石标准化值据Talyor and Mclennan, 1985)和微量元素原始地幔标准化蛛网图(b)(原始地幔标准化值据Sun and McDonough, 1989)

      Fig.  6.  Chondrite normalized REE distribution patterns (a) and primitive mantle normalized trace element spider diagrams (b) of the Binggou syeno-granite

      图  7  FeOt/MgO、(K2O+Na2O)/CaO和Zr+Nb+Ce+Y图解(底图据Whalen et al., 1987)

      A.A型花岗岩;FG.分异长英质花岗岩;OGT.未分异的M-I-S型花岗

      Fig.  7.  FeOt/MgO、(K2O+Na2O)/CaO和Zr+Nb+Ce+Y diagrams for the Binggou syeno-granite

      图  8  A/MF-C/MF图解和nK2O/nNa2O-nCaO/(nMgO+nFeOt)图解(底图分别据Altherr et al., 2000; Kaygusuz et al., 2008)

      Fig.  8.  A/MF vs.C/MF and nK2O/nNa2O vs.nCaO/(nMgO+nFeOt) diagrams for the Binggou syeno-granite

      A.Al2O3; M.MgO; F.FeOt; C.CaO

      图  9  冰沟正长花岗岩Ce/Nb-Y/Nb图解和Nb-Y-3Ga三角图解(底图据Eby,1992)

      Fig.  9.  Ce/Nb vs.Y/Nb and Nb-Y-3Ga diagrams for the Binggou syeno-granite

      表  1  冰沟粗粒正长花岗岩锆石LA-ICP-MS U-Pb定年结果

      Table  1.   Zircon LA-ICP-MS U-Pb data for Binggou alkali-feldspar granites

      点号 元素含量(×10-6) 元素比值 同位素比值 同位素年龄(Ma)
      232Th 238U Th/U 207Pb/206Pb ±1σ 207Pb/235U ±1σ 206Pb/238U ±1σ 207Pb/206Pb ±1σ 207Pb/235U ±1σ 206Pb/238U ±1σ
      1 379 507 0.75 0.073 15 0.001 44 0.597 29 0.013 18 0.059 22 0.000 99 1 018 41 476 8 371 6
      2 68 102 0.66 0.056 75 0.002 47 0.480 53 0.020 57 0.061 42 0.001 14 482 99 398 14 384 7
      3 720 923 0.78 0.057 17 0.000 91 0.493 84 0.009 18 0.062 65 0.000 94 498 36 408 6 392 6
      4 398 350 1.14 0.059 34 0.001 66 0.519 75 0.014 86 0.063 53 0.001 06 580 62 425 10 397 6
      5 773 1 110 0.70 0.054 93 0.001 21 0.475 63 0.011 45 0.062 80 0.001 05 409 50 395 8 393 6
      6 65 104 0.62 0.054 71 0.001 81 0.469 96 0.015 79 0.062 30 0.001 06 400 76 391 11 390 6
      7 66 73 0.91 0.055 23 0.003 20 0.473 33 0.026 79 0.062 16 0.001 32 422 133 393 18 389 8
      8 80 102 0.78 0.059 09 0.002 05 0.512 99 0.017 79 0.062 97 0.001 07 570 77 420 12 394 6
      9 65 70 0.92 0.055 34 0.003 06 0.473 55 0.025 64 0.062 05 0.001 28 426 127 394 18 388 8
      10 400 580 0.69 0.060 98 0.001 45 0.525 49 0.013 16 0.062 50 0.001 02 639 52 429 9 391 6
      11 309 457 0.68 0.059 08 0.001 08 0.507 23 0.010 43 0.062 27 0.000 96 570 41 417 7 389 6
      12 276 302 0.91 0.048 64 0.005 88 0.418 56 0.050 03 0.062 41 0.001 10 131 256 355 36 390 7
      13 304 452 0.67 0.059 40 0.001 38 0.535 89 0.013 03 0.065 49 0.001 02 582 52 436 9 409 6
      14 281 362 0.78 0.055 01 0.001 19 0.467 25 0.010 90 0.061 61 0.000 97 413 49 389 8 385 6
      15 74 143 0.52 0.054 04 0.001 66 0.462 11 0.014 44 0.062 06 0.001 04 373 71 386 10 388 6
      16 430 707 0.61 0.061 84 0.001 35 0.553 05 0.012 83 0.064 90 0.001 01 669 48 447 8 405 6
      17 127 140 0.91 0.054 82 0.002 49 0.474 46 0.021 38 0.062 78 0.001 27 405 104 394 15 393 8
      18 139 183 0.76 0.052 98 0.001 53 0.463 21 0.013 74 0.063 47 0.001 06 328 67 386 10 397 6
      下载: 导出CSV

      表  2  冰沟正长花岗岩主量(%)、微量(10-6)和Sr-Nd同位素测定结果

      Table  2.   Major and trace elements and Sr-Nd isotopic compositions of selected samples from the Binggou the Binggou syeno-granite

      样品号 09NM14-1 10NM17-1 10NM18-1 10NM21-11 10NM24-4 10NM25-2
      SiO2 71.85 72.37 71.77 72.12 72.77 72.20
      TiO2 0.46 0.33 0.39 0.41 0.34 0.35
      Al2O3 13.08 13.09 13.21 12.77 12.73 13.22
      Fe2O3 0.38 0.55 0.63 1.05 0.53 0.38
      FeO 3.00 2.10 2.42 1.80 2.07 2.35
      FeOt 3.34 2.59 2.99 2.74 2.55 2.69
      MnO 0.06 0.04 0.04 0.04 0.05 0.04
      MgO 0.44 0.33 0.38 0.44 0.39 0.41
      CaO 1.29 1.04 1.34 1.78 1.30 1.35
      Na2O 3.14 2.69 3.16 2.54 3.06 3.20
      K2O 5.32 5.87 5.26 5.85 5.45 5.22
      P2O5 0.09 0.06 0.07 0.07 0.06 0.08
      CO2 0.10 0.32 0.34 0.04 0.20 0.26
      H2O+ 0.59 1.05 0.83 0.91 0.89 0.78
      LOi 0.39 1.11 0.83 0.66 0.77 0.77
      Total 100.19 100.95 100.67 100.48 100.61 100.61
      A/CNK 0.99 1.03 0.99 0.93 0.96 0.99
      A/NK 1.20 1.21 1.21 1.21 1.16 1.21
      FeOt/MgO 7.60 7.86 7.86 6.24 6.53 6.57
      FeOt/(FeOt+MgO) 0.88 0.89 0.89 0.86 0.87 0.87
      Tzr(℃) 874 862 865 862 851 851
      Rb 365 329 335 342 240 376
      Sr 80 53 69 134 78 73
      Ba 572 506 483 437 492 468
      U 4.56 4.26 5.08 5.72 4.63 5.13
      Th 26.33 29.41 30.23 32.87 23.31 25.53
      Nb 25.2 21.0 24.1 21.6 17.6 27.4
      Ta 2.10 2.39 2.06 1.55 1.55 2.64
      Zr 447 356 406 453 362 353
      Hf 11.73 9.33 10.32 11.85 9.44 9.84
      Ga 21.1 23.0 23.7 20.7 22.2 25.2
      Y 79.4 69.0 67.9 69.8 57.3 94.1
      Zn 77.2 44.3 66.2 24.8 39.4 80.4
      La 60.4 81.5 85.9 88.4 60.0 78.5
      Ce 120.0 163.6 170.0 172.5 115.9 149.3
      Pr 14.68 19.54 20.29 20.56 13.31 17.02
      Nd 58.5 75.0 76.7 77.5 50.4 62.9
      Sm 12.85 13.94 14.28 14.06 9.70 13.09
      Eu 0.95 0.90 0.90 0.84 0.90 0.87
      Gd 11.74 12.97 13.37 12.93 9.17 13.03
      Tb 1.98 1.98 2.07 1.95 1.44 2.18
      Dy 12.14 11.78 11.95 10.84 8.64 14.08
      Ho 2.41 2.22 2.29 2.24 1.74 2.87
      Er 7.03 6.20 6.02 6.00 4.89 8.03
      Tm 1.03 0.91 0.91 0.87 0.71 1.25
      Yb 6.69 5.91 5.41 5.55 4.65 8.19
      Lu 0.99 0.87 0.77 0.81 0.74 1.26
      ΣREE 311.42 397.32 410.87 415.09 282.24 372.53
      LREE/HREE 6.08 8.28 8.60 9.08 7.83 6.32
      LaN/YbN 6.11 9.32 10.72 10.75 8.73 6.48
      δEu 0.23 0.20 0.20 0.19 0.29 0.20
      104 Ga/Al 3.04 3.32 3.39 3.06 3.30 3.60
      87Rb/86Sr 13.308 7 14.181 6 7.442 6 8.991 0 15.036 8
      87Sr/86Sr 0.787 700 0.729 221 0.766 885 0.772 067 0.798 207
      ±2σ 7 6 30 11 32
      (87Sr/86Sr)i 0.712 0.648 0.724 0.721 0.713
      147Sm/144Nd 0.132 3 0.112 6 0.109 7 0.116 3 0.125 8
      143Nd/144Nd 0.512 220 0.512 208 0.512 202 0.512 193 0.512 216
      ±2σ 5 3 1 2 2
      εNd(t) -4.87 -4.09 -4.06 -4.58 -4.61
      T2DM(Ga) 1.54 1.48 1.48 1.52 1.52
        注:表中氧化物含量的单位为%;稀土和微量元素单位为×10-6;全铁FeOt=0.899 81×Fe2O3+FeO;空白处表示未做测试.
      下载: 导出CSV
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