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    粤南海宴A型花岗岩与镁铁质包体的成因及意义

    贾小辉 谢国刚 孟德磊 万乐 吴俊 卜建军 吴富强 曾海良 卢加文 詹瑞华

    贾小辉, 谢国刚, 孟德磊, 万乐, 吴俊, 卜建军, 吴富强, 曾海良, 卢加文, 詹瑞华, 2018. 粤南海宴A型花岗岩与镁铁质包体的成因及意义. 地球科学, 43(7): 2294-2309. doi: 10.3799/dqkx.2018.184
    引用本文: 贾小辉, 谢国刚, 孟德磊, 万乐, 吴俊, 卜建军, 吴富强, 曾海良, 卢加文, 詹瑞华, 2018. 粤南海宴A型花岗岩与镁铁质包体的成因及意义. 地球科学, 43(7): 2294-2309. doi: 10.3799/dqkx.2018.184
    Jia Xiaohui, Xie Guogang, Meng Delei, Wan Le, Wu Jun, Bu Jianjun, Wu Fuqiang, Zeng Hailiang, Lu Jiawen, Zhan Ruihua, 2018. Petrogenesis and Implications of the Haiyan A-Type Granites and Mafic Microgranule Enclaves in Southern Guangdong Province. Earth Science, 43(7): 2294-2309. doi: 10.3799/dqkx.2018.184
    Citation: Jia Xiaohui, Xie Guogang, Meng Delei, Wan Le, Wu Jun, Bu Jianjun, Wu Fuqiang, Zeng Hailiang, Lu Jiawen, Zhan Ruihua, 2018. Petrogenesis and Implications of the Haiyan A-Type Granites and Mafic Microgranule Enclaves in Southern Guangdong Province. Earth Science, 43(7): 2294-2309. doi: 10.3799/dqkx.2018.184

    粤南海宴A型花岗岩与镁铁质包体的成因及意义

    doi: 10.3799/dqkx.2018.184
    基金项目: 

    中国地质调查局项目 DD20160064-01

    国家自然科学基金项目 41302046

    详细信息
      作者简介:

      贾小辉(1980-), 男, 助理研究员, 从事岩石学、地球化学相关研究

    • 中图分类号: P581

    Petrogenesis and Implications of the Haiyan A-Type Granites and Mafic Microgranule Enclaves in Southern Guangdong Province

    • 摘要: 华南晚中生代花岗岩及其形成的构造背景是目前研究的热点之一,通过对粤南地区A型花岗岩与镁铁质包体的年代学和地球化学组成的研究,探讨其岩石成因及构造意义.LA-ICP-MS锆石U-Pb测年结果显示,广东海宴花岗岩与镁铁质暗色微粒包体形成于早白垩世(分别为144.0±1.7 Ma和141.1±2.5 Ma).花岗岩具有典型的A型花岗岩特征:富硅、碱、铁而贫镁、钙,具有高的10 000×Ga/A1比值和Zr+Nb+Ce+Y含量等.包体具有钾玄质岩的特征:富碱更富钾、低钛、高铝及强烈富集大离子亲石元素和轻稀土元素等.花岗岩的ISr=0.706 6~0.712 2,εNdt)=-7.01~-2.03,镁铁质包体则显示了稍低的ISr(0.708 5~0.711 1)和稍高的εNdt)(-6.99~-2.23).元素及Sr-Nd同位素结果显示,花岗岩可能是中元古代地壳岩石部分熔融的产物,而钾玄质包体的初始岩浆可能源自俯冲沉积物交代的富集地幔.海宴A型花岗岩及其钾玄质包体的发现,暗示着区域早白垩世处于伸展的构造背景,不同于东南沿海地区的挤压构造应力环境.

       

    • 图  1  广东南部海宴花岗岩地质简图(a)及大地构造位置(b)

      底图据广东省地质局,1964.1:20万广海幅(F-49-XXIII)区域地质调查报告

      Fig.  1.  Geological sketch (a) and tectonic position (b) of the Haiyan granites

      图  2  海宴花岗岩(a、b)及其镁铁质暗色微粒包体(c、d)锆石U-Pb年龄谐和图

      Fig.  2.  The U-Pb concordant diagrams for the representative zircons of the Haiyan granites (a, b) and MMEs (c, d)

      图  3  SiO2 vs.主量元素图解(a、c、e~h)、A/CNK vs. A/NK图解(b)和Na2O vs. K2O图解(d)

      Fig.  3.  SiO2 vs. selected major elements diagrams (a, c, e-h), A/CNK vs. A/NK diagram (b) and Na2O vs. K2O diagram (d)

      图  4  海宴花岗岩及其镁铁质暗色包体的稀土元素分布模式(a、c)和原始地幔标准化微量元素蜘蛛网图(b、d)

      原始地幔微量元素据Sun and McDonough(1989)

      Fig.  4.  The chondrite-normalized rare earth elements (REE) (a, c) and the primitive mantle-normalized multi-element diagrams (b, d) of the Haiyan granites and MMEs

      图  5  (87Sr/86Sr)i vs. εNd(t)图解(a)和Rb vs. Sr图解(b)

      DM.亏损地幔;MORB.洋中脊玄武岩;PREMA.初始地幔;HIMU.高U/Pb比值地幔;OIB.洋岛玄武岩;BSE.地球总成分;EMI.I型富集地幔;EMII.II型富集地幔

      Fig.  5.  (87Sr/86Sr)i vs. εNd(t) diagram (a) and Rb vs. Sr diagram (b)

      图  6  A型花岗岩判别图解

      b.据Whalen et al.(1987);c.据Frost and Frost(2011);d.据Eby(1990);f.据Dall'Agnol et al.(2012)

      Fig.  6.  Discriminant diagrams of A type granite

      图  7  Ta/Yb vs. Ce/Yb(a)和Ta/Yb vs. Th/Yb关系图解(b)

      Pearce(1982)

      Fig.  7.  Ta/Yb vs. Ce/Yb (a) and Ta/Yb vs. Th/Yb diagrams (b)

      图  8  Th vs. U/Th图解(a)和Pb vs. Pb/Ce图解(b)

      图a据Hawkesworth et al.(1997);图b据Othman et al.(1989)

      Fig.  8.  Th vs. U/Th (a) and Pb vs. Pb/Ce diagrams (b)

      表  1  海宴花岗岩及其镁铁质暗色微粒包体LA-ICPMS锆石U-Pb同位素分析数据

      Table  1.   LA-ICPMS U-Pb isotopic compositions for zircons of the Haiyan granites and MMEs

      点号 Th/U Th(10-6) U(10-6) 比值 年龄(Ma)
      207Pb/206Pb ±1σ 207Pb/235U ±1σ 206Pb/238U ±1σ 207Pb/206Pb ±1σ 207Pb/235U ±1σ 206Pb/238U ±1σ
      花岗岩TK18-1
      1 0.58 182 313 0.044 66 0.002 1 0.143 24 0.007 1 0.023 18 0.000 5 37 98 136 6 148 3
      2 0.59 210 354 0.050 34 0.002 4 0.159 27 0.008 0 0.022 81 0.000 4 211 111 150 7 145 2
      3 0.45 178 391 0.045 98 0.002 5 0.151 07 0.008 8 0.024 06 0.000 5 3 117 143 8 153 3
      4 0.64 298 467 0.049 48 0.002 1 0.156 92 0.006 4 0.023 08 0.000 4 170 88 148 6 147 3
      5 0.45 179 399 0.047 97 0.002 4 0.154 33 0.007 6 0.023 29 0.000 4 98 105 146 7 148 2
      6 0.57 270 477 0.050 83 0.002 2 0.156 16 0.006 3 0.022 28 0.000 3 233 89 147 6 142 2
      7 0.40 158 391 0.051 49 0.003 1 0.160 83 0.010 5 0.022 44 0.000 5 263 142 151 9 143 3
      8 0.45 160 354 0.047 07 0.002 2 0.148 53 0.007 1 0.022 65 0.000 4 53 100 141 6 144 2
      9 0.47 94 200 0.051 82 0.003 2 0.159 50 0.009 6 0.022 88 0.000 5 278 132 150 8 146 3
      10 0.83 457 553 0.047 31 0.002 1 0.146 05 0.006 6 0.022 13 0.000 4 65 93 138 6 141 2
      11 0.64 357 555 0.047 71 0.001 6 0.148 35 0.005 3 0.022 15 0.000 4 85 71 140 5 141 2
      12 0.45 100 225 0.052 48 0.002 9 0.161 87 0.008 7 0.023 12 0.000 5 306 115 152 8 147 3
      13 0.29 328 1 118 0.047 88 0.001 7 0.171 16 0.006 1 0.025 62 0.000 4 93 74 140 3 143 3
      14 0.58 469 802 0.048 57 0.001 6 0.149 60 0.005 1 0.021 97 0.000 3 127 74 142 4 140 2
      15 0.55 265 478 0.046 05 0.005 3 0.135 90 0.015 4 0.021 41 0.000 4 - 229 129 14 137 3
      16 0.44 183 413 0.049 64 0.002 3 0.151 45 0.006 7 0.022 30 0.000 4 178 94 143 6 142 3
      17 0.35 182 528 0.053 17 0.002 8 0.154 05 0.006 7 0.021 40 0.000 4 336 93 145 6 136 2
      18 0.45 131 288 0.051 76 0.002 6 0.158 36 0.007 4 0.022 45 0.000 4 275 101 149 7 143 3
      19 0.81 495 612 0.050 19 0.002 4 0.160 14 0.007 8 0.023 22 0.000 4 204 106 151 7 148 3
      20 0.50 182 362 0.046 89 0.002 1 0.148 21 0.006 4 0.022 91 0.000 4 43 85 140 6 146 3
      镁铁质暗色微粒包体TK17-3
      1 0.55 1 048 1 922 0.047 71 0.001 7 0.143 46 0.005 1 0.021 50 0.000 4 85 70 136 4 137 2
      2 0.18 1 073 5 805 0.047 89 0.001 3 0.141 91 0.004 0 0.021 13 0.000 3 94 57 135 4 135 2
      3 0.64 2 883 4 539 0.047 97 0.001 4 0.150 82 0.004 3 0.022 44 0.000 3 98 59 143 4 143 2
      4 0.34 1 186 3 493 0.047 00 0.001 3 0.141 20 0.004 0 0.021 41 0.000 3 49 54 134 4 137 3
      5 0.45 1 311 2 934 0.048 85 0.001 3 0.147 84 0.004 0 0.021 68 0.000 3 141 53 140 3 138 2
      6 0.71 4 180 5 887 0.047 45 0.001 1 0.141 89 0.003 4 0.021 35 0.000 3 72 48 135 3 136 2
      7 0.26 677 2 633 0.048 25 0.001 5 0.150 31 0.004 3 0.022 34 0.000 3 112 61 142 4 142 2
      8 0.24 779 3 212 0.047 76 0.001 3 0.144 28 0.003 9 0.021 57 0.000 3 87 56 137 3 138 2
      9 0.15 1 007 6 638 0.047 46 0.001 2 0.151 55 0.004 0 0.022 73 0.000 3 72 53 143 3 145 2
      10 0.55 2 364 4 317 0.050 75 0.001 4 0.160 80 0.004 7 0.022 59 0.000 3 229 60 151 4 144 2
      11 0.71 2 635 3 733 0.047 30 0.001 5 0.136 06 0.004 3 0.020 56 0.000 3 64 62 130 4 131 2
      12 0.85 4 900 5 779 0.047 40 0.001 2 0.141 38 0.003 6 0.021 28 0.000 3 69 51 134 3 136 2
      13 0.82 5 932 7 231 0.046 53 0.001 1 0.143 10 0.003 3 0.022 00 0.000 3 25 40 136 3 140 2
      14 0.20 724 3 579 0.045 86 0.001 1 0.138 27 0.003 4 0.021 54 0.000 3 10 40 131 3 137 2
      15 1.05 7 966 7 579 0.047 77 0.001 0 0.152 21 0.003 2 0.022 75 0.000 3 88 42 144 3 145 3
      16 0.67 2 373 3 529 0.047 67 0.001 2 0.140 70 0.003 6 0.021 11 0.000 3 83 51 134 3 135 2
      17 0.27 840 3 122 0.048 97 0.001 2 0.160 62 0.004 1 0.023 39 0.000 3 147 51 151 4 149 2
      18 0.37 944 2 579 0.046 72 0.001 3 0.149 38 0.004 2 0.022 85 0.000 3 35 52 141 4 146 2
      19 0.41 1 396 3 383 0.048 59 0.001 2 0.155 47 0.003 9 0.022 86 0.000 3 128 52 147 3 146 3
      20 1.02 6 490 6 360 0.052 85 0.001 3 0.150 53 0.003 6 0.020 41 0.000 3 323 44 142 3 130 2
      下载: 导出CSV

      表  2  海宴花岗岩及其镁铁质暗色微粒包体主量元素(%)和微量元素(10-6)分析结果

      Table  2.   Major (%) and trace elements (10-6) of the Haiyan granites and MMEs

      样品 花岗岩 镁铁质暗色包体
      TK17-1 TK17-2 TK19-1 TK18-1 TK18-2 TK17-3 TK17-4 TK17-5 TK18-3
      SiO2 73.16 72.91 73.63 66.63 67.46 68.64 68.47 66.47 66.50
      Al2O3 12.91 12.81 13.10 14.88 14.46 14.41 14.52 12.36 14.93
      Fe2O3 0.91 0.49 0.08 2.28 1.15 0.63 1.11 2.12 1.24
      FeO 2.07 3.11 2.64 2.64 3.79 3.37 2.96 5.84 3.81
      CaO 1.02 1.11 1.41 2.81 2.53 1.47 1.52 1.54 2.36
      MgO 0.34 0.34 0.22 1.03 1.06 0.50 0.52 1.24 0.89
      K2O 4.81 4.66 4.83 4.53 3.95 5.16 4.89 3.94 5.03
      Na2O 3.45 3.50 3.08 3.04 3.04 4.06 4.09 3.08 2.80
      TiO2 0.23 0.22 0.20 0.58 0.62 0.33 0.34 0.88 0.64
      P2O5 0.08 0.08 0.05 0.23 0.23 0.11 0.11 0.22 0.20
      MnO 0.09 0.07 0.05 0.11 0.10 0.11 0.11 0.22 0.09
      灼失 0.55 0.19 0.24 0.72 0.99 0.65 0.82 1.22 0.84
      Li 38.4 50.7 23.3 35.0 29.9 46.4 46.5 142 30.4
      Sc 1.47 1.58 2.39 7.28 5.97 2.13 2.49 2.71 6.99
      V 8.03 7.71 6.77 48.8 55.9 11.1 12.3 27.8 42.6
      Cr 21.40 5.94 8.28 5.81 6.40 19.2 21.2 9.25 35.2
      Co 2.48 2.54 2.67 6.78 6.96 4.09 4.30 6.02 7.04
      Ni 4.07 3.30 4.04 3.73 3.00 3.62 3.92 8.79 6.34
      Cu 9.28 6.54 7.74 6.14 9.65 10.0 11.2 15.6 10.5
      Zn 28.3 30.1 34.8 72.3 71.7 42.8 43.3 101 63.1
      Ga 16.4 15.9 20.8 18.8 19.4 20.7 20.7 19.5 25.2
      Rb 234 220 134 58.1 47.4 230 221 80.4 96.0
      Sr 104 104 105 326 284 138 150 83.2 262
      Y 29.8 28.4 20.2 23.5 29.9 24.9 26.8 44.4 47.9
      Zr 200 166 213 251 234 269 267 590 392
      Nb 44.0 42.5 9.81 15.2 17.1 42.6 45.8 108 23.0
      Mo 1.04 0.80 2.93 0.91 0.65 1.95 2.02 3.26 1.28
      Sb 0.23 0.11 0.43 0.17 0.31 0.38 0.65 0.24 0.11
      Cs 7.30 10.5 3.05 4.25 4.39 9.04 9.69 12.3 6.35
      Ba 248 261 524 559 485 490 465 162 822
      La 49.4 53.0 59.0 53.5 52.8 77.9 61.3 117 88.3
      Ce 91.4 98.0 115 101 99.6 136 110 226 110
      Pr 8.70 9.20 11.6 10.1 10.5 11.9 10.3 20.8 17.8
      Nd 29.3 30.1 40.5 37.0 38.9 37.4 33.6 67.5 66.2
      Sm 5.10 5.15 6.78 6.54 7.32 5.53 5.36 10.4 11.9
      Eu 0.64 0.63 1.11 1.52 1.59 0.91 0.92 0.48 2.36
      Gd 4.80 4.84 5.91 6.00 6.56 5.34 5.14 9.64 10.5
      Tb 0.80 0.75 0.83 0.89 1.02 0.74 0.76 1.34 1.65
      Dy 4.95 4.66 4.45 4.90 5.84 4.29 4.54 7.66 9.53
      Ho 1.08 1.00 0.85 0.96 1.18 0.91 0.97 1.62 1.88
      Er 3.33 3.19 2.30 2.62 3.21 2.76 3.00 4.92 5.01
      Tm 0.62 0.60 0.34 0.40 0.50 0.51 0.55 0.86 0.76
      Yb 4.58 4.50 2.12 2.53 3.29 3.75 3.98 6.14 4.94
      Lu 0.66 0.67 0.28 0.35 0.45 0.56 0.59 0.93 0.66
      Hf 6.13 5.04 5.73 6.31 6.04 7.37 7.17 15.50 9.76
      Ta 5.87 6.27 0.88 0.99 1.20 4.79 5.64 8.36 1.50
      W 2.93 6.86 2.43 0.97 1.87 3.07 9.47 22.3 1.73
      Pb 15.8 46.1 64.6 17.7 49.6 39.7 49.8 11.6 23.0
      Th 19.0 24.0 13.5 13.6 11.6 23.9 23.6 158 13.5
      U 8.57 10.1 1.99 2.42 3.04 8.59 9.53 36.4 2.42
      下载: 导出CSV

      表  3  海宴花岗岩及其镁铁质暗色微粒包体Sr-Nd同位素分析结果

      Table  3.   Sr-Nd isotopic compositions of the Haiyan granites and MMEs

      样品号 岩性 Sm(10-6) Nd(10-6) 147Sm/144Nd 143Nd/144Nd 2σ T(Ma) εNd(t) TDM2(Ga) Rb(10-6) Sr(10-6) 87Rb/86Sr 87Sr/86Sr 2σ T(Ma) (87Sr/86Sr)i
      TK17-1 花岗岩 5.1 29.3 0.105 7 0.512 448 0.000 006 144 -2.03 1.11 339 114 8.398 0.723 770 0.000 010 144 0.706 6
      TK18-1 花岗岩 6.5 37.8 0.105 0 0.512 266 0.000 006 144 -5.57 1.40 198 336 1.658 0.712 660 0.0000 08 144 0.709 3
      TK19-1 花岗岩 6.8 41.3 0.099 2 0.512 187 0.000 008 144 -7.01 1.52 177 109 4.562 0.721 540 0.000 010 144 0.712 2
      TK17-5 包体 9.9 64.9 0.092 8 0.512 426 0.000 008 144 -2.23 1.12 347 83.8 11.673 0.732 410 0.000 008 144 0.708 5
      TK18-3 包体 11.9 66.5 0.108 6 0.512 197 0.000 008 144 -6.99 1.51 235 287 2.312 0.715 790 0.000 006 144 0.711 1
      注:TDM2值采用Depaolo et al.(1991)两阶段模式年龄.
      下载: 导出CSV
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