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    南岭九嶷山地区砂子岭岩体成因与构造属性:来自锆石U-Pb年代学、岩石地球化学及Sr、Nd、Hf同位素证据

    李剑锋 付建明 马昌前 卢友月 程顺波 马丽艳 秦拯纬

    李剑锋, 付建明, 马昌前, 卢友月, 程顺波, 马丽艳, 秦拯纬, 2020. 南岭九嶷山地区砂子岭岩体成因与构造属性:来自锆石U-Pb年代学、岩石地球化学及Sr、Nd、Hf同位素证据. 地球科学, 45(2): 374-388. doi: 10.3799/dqkx.2019.013
    引用本文: 李剑锋, 付建明, 马昌前, 卢友月, 程顺波, 马丽艳, 秦拯纬, 2020. 南岭九嶷山地区砂子岭岩体成因与构造属性:来自锆石U-Pb年代学、岩石地球化学及Sr、Nd、Hf同位素证据. 地球科学, 45(2): 374-388. doi: 10.3799/dqkx.2019.013
    Li Jianfeng, Fu Jianming, Ma Changqian, Lu Youyue, Cheng Shunbo, Ma Liyan, Qin Zhengwei, 2020. Petrogenesis and Tectonic Setting of the Shaziling Pluton in Jiuyishan Area, Nanling: Evidence from Zircon U-Pb Geochronology, Petrogeochemistry, and Sr-Nd-Hf Isotopes. Earth Science, 45(2): 374-388. doi: 10.3799/dqkx.2019.013
    Citation: Li Jianfeng, Fu Jianming, Ma Changqian, Lu Youyue, Cheng Shunbo, Ma Liyan, Qin Zhengwei, 2020. Petrogenesis and Tectonic Setting of the Shaziling Pluton in Jiuyishan Area, Nanling: Evidence from Zircon U-Pb Geochronology, Petrogeochemistry, and Sr-Nd-Hf Isotopes. Earth Science, 45(2): 374-388. doi: 10.3799/dqkx.2019.013

    南岭九嶷山地区砂子岭岩体成因与构造属性:来自锆石U-Pb年代学、岩石地球化学及Sr、Nd、Hf同位素证据

    doi: 10.3799/dqkx.2019.013
    基金项目: 

    中国地质调查局项目"南岭成矿带中西段地质矿产调查" 121201009000150002

    详细信息
      作者简介:

      李剑锋(1986-), 男, 助理研究员, 博士后, 主要从事矿床学研究工作

      通讯作者:

      付建明

    • 中图分类号: P597

    Petrogenesis and Tectonic Setting of the Shaziling Pluton in Jiuyishan Area, Nanling: Evidence from Zircon U-Pb Geochronology, Petrogeochemistry, and Sr-Nd-Hf Isotopes

    • 摘要: 九嶷山地区砂子岭岩体作为南岭花岗岩带的有机组成部分,对其主要岩石类型开展了年代学研究,系统的LA-ICP-MS锆石定年结果表明,含斑中细粒花岗闪长岩成岩年龄为151.9±1.1 Ma、152.1±1.1 Ma,中细粒斑状二长花岗岩成岩年龄为154.1±1.2 Ma;确定其成岩年代为燕山早期,而不是以前普遍认为的印支期.岩石地球化学分析显示,砂子岭岩体具有富硅碱贫钙镁、K2O/Na2O为1.37~2.65、准铝-过铝质(0.93~1.09),FeO*/MgO比值大(5.43~15.33,平均7.14)等特点;岩石稀土含量介于186.75×10-6~413.17×10-6之间,明显高于世界花岗岩均值,稀土元素配分曲线呈右倾轻稀土富集型,具明显铕负异常,δEu值为0.095~0.224;岩石富集Ga、Y、Nb、Zr、Hf等大离子高场强元素及亏损Ni、Cr、Eu、Ti、V、P、Sr等元素,Ga/Al比值为245×10-6~582×10-6(平均值350×10-6)、Zr+Nb+Ce+Y为256.8×10-6~630.7×10-6(平均值441.95×10-6),显示A型花岗岩地球化学属性,形成于伸展构造体系的造山后环境.Sr、Nd、Hf同位素显示砂子岭岩体具较高Sr同位素初始值(ISr=0.716 03~0.718 17),较低的εNdt)(-6.8~-7.4)、εHft)(4.8~-14.2)值特点;揭示其源区为地壳杂砂岩/泥质岩的部分熔融,成岩过程中有地幔物质的贡献;钕、铪模式年龄较接近,分别为1 498~1 546 Ma与1 061~1 756 Ma,暗示其源岩从地幔储库中脱离的时间为中元古代.结合南岭地区地质演化史,中生代九嶷山地区恰处于板块拼合带及太平洋板块弧后伸展的构造背景之下,具发生过岛弧岩浆作用、构造相对薄弱且存在大量具较高Lu-Hf、Sm-Nd同位素比值新生地壳物质的特点;地幔对流与软流圈上涌引发源区部分熔融形成具有类似同位素组成特征的A型花岗岩,即为砂子岭及九嶷山复式岩体的成因.

       

    • 图  1  九嶷山地区地质简图

      图a中S、M、N分别为南岭南、中、北花岗岩带;1.白垩系;2.石炭系;3.泥盆系;4.寒武系;5.震旦系;6.志留纪花岗岩;7.中侏罗世花岗岩;8.中侏罗世碎斑熔岩;9.中侏罗世英安/流纹(斑)岩;10.岩相界线;11.地质界线;12.不整合界线;13.断层;14.取样位置

      Fig.  1.  Simplified geological map of Jiuyishan

      图  2  砂子岭岩体(a)、暗色包体(b)、(c)及显微照片(d)、(e)、(f)

      a.样品12D72采样位置,见有椭圆-不规则状暗色包体;b.暗色包体;c. 13D13采样点,寄主岩石为中细粒斑状二长花岗岩;d.含斑中细粒花岗闪长岩(12D72,正交偏光);e.斜长石环带(12D72,正交偏光);f.中细粒斑状二长花岗岩(12D72,正交偏光);矿物代码: Hb.角闪石; Bi.黑云母; Pl.斜长石; Q.石英.

      Fig.  2.  Shaziling rock mass (a) MME (b)、(c) and its microscopic photos (d)、(e)、(f)

      图  3  研究区岩浆岩锆石U-Pb年龄谐和图和锆石阴极发光(CL)图像

      Fig.  3.  Magmatite Zircon U-Pb Concordia diagrams for the CL images in the study area

      图  4  砂子岭岩体Na2O+K2O/SiO2(a)、K2O-SiO2图解(b)和A/NK-A/KNC图解(c)

      Fig.  4.  The Na2O+K2O/SiO2(a)、K2O-SiO2 (b) and A/NK-A/KNC diagram (c) of Shaziling rock mass

      图  5  砂子岭岩体REE配分图(a)和微量元素蛛网图(b)

      Fig.  5.  Chondrite-normalized REE patterns and primitive mantle-normalized spidergrams of Shaziling

      图  6  砂子岭岩体εNd(t)-Isr、εHf(t)-Age、CaO/(MgO+FeO)-Al2O3/(MgO+FeO)及Rb/Sr-Rb/Ba图解

      Fig.  6.  εNd(t)-Isr、εHf(t)-Age、CaO/(MgO+FeO)-Al2O3/(MgO+FeO) and Rb/Sr-Rb/Ba diagrams of Shaziling

      图  7  砂子岭岩体(10 000×Ga/Al)vs(FeO*/MgO)/Ce /[(Na2O+K2O)/CaO]、(Zr+Nb+Ce+Y)vs(FeO*/MgO)、Nb-Y-Ce及Nb-Y-Ga判别图解(底图据Whalen et al., 1987)

      Fig.  7.  (10 000×Ga/Al)vs(FeO*/MgO)/Ce/[(Na2O+K2O)/CaO]、(Zr+Nb+Ce+Y)VS(FeO*/MgO)、Nb-Y-Ce and Nb-Y-Ga discrimination diagrams of Shaziling rock mass

      表  3  砂子岭岩体Sr-Nd同位素数据

      Table  3.   Nd-Sr-Pb isotopic data for Xishan volcanic-intrusive complex rocks

      样号 Rb(10-6) Sr(10-6) 87Rb/86Sr 87Sr/86Sr 误差2σ I(Sr) εSr(0) εSr(t) fRb/Sr Sm(10-6) Nd(10-6) 147Sm/134Nd 143Nd/144Nd 误差2σ INd εNd(t) T2DM fSm/Nd
      D116-1 290.1 86.9 9.652 0.737 82 0.000 001 0.716 28 473.0 169.9 115.71 9.180 36.55 0.151 9 0.512 215 0.000 012 0.512 059 -7.36 1 541 -0.23
      D117-1 196.1 135.2 4.188 0.726 79 0.000 009 0.717 44 316.4 186.4 49.64 10.290 49.53 0.125 7 0.512 190 0.000 070 0.512 061 -7.32 1 542 -0.36
      D118-1 188.6 137.6 3.959 0.726 39 0.000 003 0.717 55 310.7 187.9 46.87 10.310 51.17 0.121 8 0.512 183 0.000 060 0.512 058 -7.38 1 546 -0.38
      12D72 166.8 145.2 3.318 0.724 86 0.000 005 0.717 59 289.0 188.4 39.12 14.370 86.74 0.100 2 0.512 168 0.000 010 0.512 067 -7.27 1 537 -0.49
      12D73 222.1 120.0 5.347 0.727 74 0.000 001 0.716 03 329.9 166.3 63.66 9.417 48.29 0.118 0 0.512 210 0.000 040 0.512 091 -6.80 1 498 -0.40
      13D13 196.3 118.2 4.799 0.728 68 0.000 004 0.718 17 343.2 196.7 57.03 11.790 64.36 0.110 8 0.512 180 0.000 060 0.512 068 -7.25 1 535 -0.44
      下载: 导出CSV

      表  4  砂子岭岩体Hf同位素数据

      Table  4.   Hf isotopic data for Xishan volcanic-intrusive complex rocks

      测点号 176Hf/177Hf 176Lu/177Hf 176Yb/177Hf εHf(0) Age εHf(t) TDM T2DM
      12D72-01 0.282 624 0.000 013 0.000 806 0.025 352 -5.2 153 -2.0 0.5 886 38 1 326 60
      12D72-02 0.282 445 0.000 019 0.000 858 0.026 673 -11.5 151 -8.3 0.7 1 137 52 1 726 83
      12D72-03 0.282 630 0.000 014 0.001 153 0.036 333 -5.0 152 -1.8 0.5 885 39 1 313 62
      12D72-04 0.282 463 0.000 010 0.001 318 0.042 661 -10.9 151 -7.8 0.3 1 127 28 1 691 44
      12D72-05 0.282 513 0.000 019 0.001 392 0.043 024 -9.1 151 -6.0 0.7 1 057 53 1 577 84
      12D72-06 0.282 816 0.000 013 0.001 095 0.034 853 1.6 154 4.8 0.4 620 36 894 57
      12D72-07 0.282 744 0.000 011 0.001 654 0.052 192 -1.0 152 2.2 0.4 733 32 1 061 49
      12D72-08 0.282 603 0.000 012 0.000 951 0.030 035 -6.0 155 -2.7 0.4 918 33 1 371 53
      12D72-09 0.282 557 0.000 009 0.000 865 0.027 294 -7.6 152 -4.3 0.3 980 26 1 475 42
      12D72-10 0.282 593 0.000 008 0.001 011 0.027 185 -6.3 151 -3.1 0.3 934 24 1 397 38
      12D72-11 0.282 278 0.000 017 0.000 630 0.015 328 -17.5 153 -14.2 0.6 1 362 47 2 097 75
      12D72-12 0.282 600 0.000 020 0.000 940 0.024 645 -6.1 434 3.2 0.7 922 55 1 212 88
      12D72-13 0.282 600 0.000 013 0.000 853 0.021 819 -6.1 151 -2.9 0.5 921 37 1 381 59
      12D72-14 0.282 607 0.000 009 0.000 991 0.026 542 -5.8 151 -2.6 0.3 914 26 1 365 42
      12D72-15 0.282 557 0.000 013 0.000 650 0.016 865 -7.6 151 -4.4 0.5 975 38 1 475 60
      12D72-16 0.282 507 0.000 010 0.000 899 0.023 017 -9.4 154 -6.1 0.4 1 052 28 1 588 45
      12D72-17 0.282 560 0.000 012 0.000 864 0.022 860 -7.5 152 -4.3 0.4 977 34 1 469 54
      12D72-18 0.282 620 0.000 011 0.000 662 0.017 171 -5.4 151 -2.1 0.4 888 32 1 335 51
      12D72-19 0.282 431 0.000 015 0.000 696 0.018 064 -12.1 154 -8.8 0.5 1 152 42 1 756 67
      12D72-20 0.282 672 0.000 008 0.000 835 0.021 963 -3.5 154 -0.2 0.3 818 23 1 216 37
      下载: 导出CSV
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