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    苏门答腊岛北部Takengon早志留世S型花岗片麻岩年代学、地球化学特征及构造意义

    徐畅 王岳军 钱鑫 张玉芝 余小清

    徐畅, 王岳军, 钱鑫, 张玉芝, 余小清, 2020. 苏门答腊岛北部Takengon早志留世S型花岗片麻岩年代学、地球化学特征及构造意义. 地球科学, 45(6): 2077-2090. doi: 10.3799/dqkx.2020.030
    引用本文: 徐畅, 王岳军, 钱鑫, 张玉芝, 余小清, 2020. 苏门答腊岛北部Takengon早志留世S型花岗片麻岩年代学、地球化学特征及构造意义. 地球科学, 45(6): 2077-2090. doi: 10.3799/dqkx.2020.030
    Xu Chang, Wang Yuejun, Qian Xin, Zhang Yuzhi, Yu Xiaoqing, 2020. Geochronological and Geochemical Characteristics of Early Silurian S-Type Granitic Gneiss in Takengon Area of Northern Sumatra and Its Tectonic Implications. Earth Science, 45(6): 2077-2090. doi: 10.3799/dqkx.2020.030
    Citation: Xu Chang, Wang Yuejun, Qian Xin, Zhang Yuzhi, Yu Xiaoqing, 2020. Geochronological and Geochemical Characteristics of Early Silurian S-Type Granitic Gneiss in Takengon Area of Northern Sumatra and Its Tectonic Implications. Earth Science, 45(6): 2077-2090. doi: 10.3799/dqkx.2020.030

    苏门答腊岛北部Takengon早志留世S型花岗片麻岩年代学、地球化学特征及构造意义

    doi: 10.3799/dqkx.2020.030
    基金项目: 

    国家自然科学基金项目 41830211

    国家自然科学基金项目 U1701641

    国家重点研发计划项目 2016YFC0600303

    广东省基础与应用基础研究基金 2018B030312007

    广东省基础与应用基础研究基金 2019B1515120019

    详细信息
      作者简介:

      徐畅(1996-), 男, 硕士研究生, 从事岩石大地构造和岩石地球化学的研究.ORCID:0000-0001-9590-9329.E-mail:xuch33@mail2.sysu.edu.cn

      通讯作者:

      钱鑫, E-mail:qianx3@mail.sysu.edu.cn

    • 中图分类号: P545

    Geochronological and Geochemical Characteristics of Early Silurian S-Type Granitic Gneiss in Takengon Area of Northern Sumatra and Its Tectonic Implications

    • 摘要: 苏门答腊岛位于巽他大陆西南缘,被中苏门答腊构造带分隔为东、西苏门答腊两地体.其中东苏门答腊地体的基底年龄和构造归属均未得到很好地约束.在东苏门答腊北部Takengon地区新识别出的花岗片麻岩进行了锆石U-Pb年代学、原位Hf同位素和全岩地球化学研究.年代学结果表明该套花岗片麻岩的206Pb/238U加权平均年龄为442 ±5 Ma(MSWD=1.03),代表其结晶年龄.锆石的εHft)介于-1.3至-7.8之间.地球化学研究表明,样品富SiO2(69.97%~74.30%)和Al2O3(13.90%~15.93%),相对贫TiO2(0.48%~0.61%)、MgO(0.54%~0.93%)和CaO(0.11%~0.25%).样品具高的A/CNK值(2.58~3.06)和CIPW刚玉体积百分含量(10.0%~11.4%),具有S型花岗岩的特征.其轻重稀土分异明显,富集LILE(Rb、Th、U),亏损HFSE(Nb、Ta、Ti).地球化学研究表明Takengon花岗片麻岩是变沉积岩部分熔融形成的.该套花岗片麻岩的发现证实了在东苏门答腊地块发育有前志留世基底岩石,其形成与原特提斯洋的演化有关.

       

    • 图  1  区域构造简图(a)和苏门答腊北部地质简图与采样点位置(b)

      Wang et al.(2016, 2018)修改

      Fig.  1.  Simplified geological map with tectonic frame of the region (a) and simplified geological map of northern Sumatra (b)

      图  2  苏门答腊Takengon花岗片麻岩样品野外照片(a)和显微照片(b, c)

      Q.石英;Kfs.钾长石;Ms.白云母

      Fig.  2.  Outcrop (a) and micrographic photos (b, c) of granitic gneissic samples from Takengon in Sumatra

      图  3  苏门答腊Takengon花岗片麻岩代表性锆石颗粒的阴极发光图像及其206Pb/238U年龄和εHf(t)值

      Fig.  3.  Cathodoluminescence (CL) image of representative zircon grains with their 206Pb/238U ages and εHf (t) values from the Takengon granitic gneissic samples in Sumatra

      图  4  Takengon花岗片麻岩的锆石U-Pb年龄谐和图和加权平均年龄图(a)、锆石U-Th图解(b)和锆石稀土元素球粒陨石标准化图解(c)

      Fig.  4.  Concordia and weighted mean age diagram of zircon U versus Pb data (a), Th-U diagram of zircon trace elements data (b) and chondrite-normalized REE diagram of zircons (c) for the representative samples of Takengon granitic gneissic

      图  5  苏门答腊Takengon花岗片麻岩样品的QAP图解(a)、CaO-FeOT+MgO-Al2O3-(Na2O+K2O)图解(b)、FeOT/MgO-10 000×Ga/Al图解(c)和10000×Ga/Al-(Zr+Nb+Ce+Y)图解(d)

      Fig.  5.  QAP diagram (a), CaO-FeOT+MgO-Al2O3-(Na2O+K2O) diagram (b), FeOT/MgO-10 000×Ga/Al diagram (c) and 10 000×Ga/Al-(Zr+Nb+Ce+Y) diagram (d) diagrams for the Takengon granitic gneissic samples in Sumatra

      图  6  苏门答腊Takengon花岗片麻岩的稀土元素球粒陨石标准化配分图(a)和微量元素原始地幔标准化蛛网图(b)

      球粒陨石标准化数据据Sun and McDonough(1989);原始地幔标准化数据据Taylor and McLennan(1985);滇西北和喜马拉雅早古生代花岗岩数据据Chen et al.(2007), 张泽明等(2008), Liu et al.(2009), 时超等(2010)Zhang et al.(2012)

      Fig.  6.  The patterns of the chondrite-normalized REE diagram (a) and primitive mantle-normalized trace elements spidergram (b) for the Takengon granitic gneissic in Sumatra

      图  7  苏门答腊Takengon花岗片麻岩样品的Rb/Sr-Rb/Ba图解(a)和稀土元素部分熔融模拟(b)

      Lachlan褶皱带和喜马拉雅强过铝花岗岩数据和端元混合曲线据Sylvester (1998); 南羌塘平均上地壳沉积岩数据据Gao et al. (1998),元素配分系数和矿物含量百分比数据据Hanson (1980);(a)中底图转引自Wang et al. (2016)

      Fig.  7.  Rb/Sr versus Rb/Ba (a) and simulation of partial melting for REE (b) for the Takengon granitic gneissic samples in Sumatra

      图  8  苏门答腊Takengon花岗片麻岩的锆石εHf(t)-年龄图解(a、b)

      苏门答腊碎屑锆石数据据Zhang et al.(2018);滇缅泰板块早古生代花岗质岩石数据据Chen et al.(2007)Liu et al.(2009)董美玲等(2012)Wang et al.(2013)蔡志慧等(2013)邢晓婉等(2015)康欢等(2016)崔晓琳等(2017)

      Fig.  8.  Zircon εHf (t) versus age diagram of Takengon granitic gneiss in Sumatra (a, b)

      图  9  滇缅泰板块早古生代花岗质岩石年龄及构造背景

      图中数据参考文献见Chen et al.(2007)Liu et al.(2009)董美玲等(2012)李再会等(2012)刘琦胜等(2012)熊昌利等(2012)Wang et al.(2013)蔡志慧等(2013)邢晓婉等(2015)Shi et al.(2016)康欢等(2016)崔晓琳等(2017)

      Fig.  9.  Summary of age and tectonic settings data of the Early Paleozoic granitic rocks in the Sibumasu block

      表  1  苏门答腊Takengon花岗片麻岩样品全岩主量元素(%)和微量元素(10-6)分析结果

      Table  1.   Major and trace elements analytical results for the Takengon granitic gneissic samples in Sumatra

      样品号 18SM-23-3 18SM-23-4 18SM-23-5 18SM-23-6 18SM-23-7
      SiO2 71.80 69.97 70.12 74.30 71.14
      TiO2 0.53 0.61 0.48 0.58 0.53
      Al2O3 14.62 15.76 13.93 13.90 15.26
      Fe2O3T 3.54 3.80 5.20 3.65 3.65
      MnO 0.04 0.05 0.06 0.02 0.07
      MgO 0.61 0.85 0.93 0.54 0.55
      CaO 0.18 0.24 0.25 0.11 0.17
      Na2O 0.10 0.10 0.10 0.02 0.09
      K2O 4.77 4.68 4.25 3.97 4.79
      P2O5 0.15 0.17 0.15 0.07 0.15
      LOI 3.44 3.62 3.83 3.08 3.58
      Total 99.80 99.85 99.31 100.24 99.97
      A/CNK 2.58 2.77 2.66 3.06 2.70
      A/NK 2.71 2.98 2.89 3.20 2.85
      Sc 8.04 10.1 8.40 8.57 7.74
      V 48.0 60.0 45.0 51.0 48.0
      Cr 18.0 22.0 17.0 36.0 16.0
      Co 4.63 5.57 5.36 7.12 4.99
      Ni 4.62 5.55 7.18 5.81 5.16
      Ga 18.9 23.8 18.5 19.7 19.8
      Rb 167 202 167 147 173
      Sr 27.2 14.0 27.1 52.3 24.0
      Y 26.1 35.2 31.9 28.8 32.8
      Zr 207 229 201 238 202
      Nb 13.2 16.6 12.2 13.9 13.4
      Cs 8.70 11.6 12.6 5.03 7.00
      Ba 634 539 598 711 554
      La 32.4 33.2 28.8 46.0 45.1
      Ce 66.4 70.2 60.1 94.6 91.1
      Pr 8.29 8.81 7.62 11.8 11.4
      Nd 31.3 33.7 28.9 44.4 42.1
      Sm 5.89 6.88 5.96 7.97 8.23
      Eu 0.84 0.88 0.88 0.88 1.04
      Gd 5.43 6.54 5.78 6.94 7.30
      Tb 0.91 1.16 1.00 1.08 1.19
      Dy 5.39 7.19 6.05 6.04 6.86
      Ho 1.11 1.52 1.29 1.25 1.39
      Er 3.31 4.58 3.95 3.77 4.10
      Tm 0.54 0.72 0.64 0.58 0.63
      Yb 3.51 4.73 4.18 3.91 4.12
      Lu 0.53 0.74 0.65 0.59 0.61
      Hf 7.46 8.40 7.11 8.66 7.28
      Ta 1.32 1.60 1.24 1.17 1.40
      Pb 2403 2737 3041 1239 1316
      Th 16.5 18.0 15.7 13.6 16.1
      U 3.41 3.31 2.78 3.48 2.33
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