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    辽东岫岩晚侏罗世荒地岩体的地球化学、年代学与Hf同位素及构造意义

    薛吉祥 刘正宏 刘杰勋 董晓杰 冯帆 连光辉

    薛吉祥, 刘正宏, 刘杰勋, 董晓杰, 冯帆, 连光辉, 2020. 辽东岫岩晚侏罗世荒地岩体的地球化学、年代学与Hf同位素及构造意义. 地球科学, 45(6): 2030-2043. doi: 10.3799/dqkx.2020.008
    引用本文: 薛吉祥, 刘正宏, 刘杰勋, 董晓杰, 冯帆, 连光辉, 2020. 辽东岫岩晚侏罗世荒地岩体的地球化学、年代学与Hf同位素及构造意义. 地球科学, 45(6): 2030-2043. doi: 10.3799/dqkx.2020.008
    Xue Jixiang, Liu Zhenghong, Liu Jiexun, Dong Xiaojie, Feng Fan, Lian Guanghui, 2020. Geochemistry, Geochronology, Hf Isotope and Tectonic Significance of Late Jurassic Huangdi Pluton in Xiuyan, Liaodong Peninsula. Earth Science, 45(6): 2030-2043. doi: 10.3799/dqkx.2020.008
    Citation: Xue Jixiang, Liu Zhenghong, Liu Jiexun, Dong Xiaojie, Feng Fan, Lian Guanghui, 2020. Geochemistry, Geochronology, Hf Isotope and Tectonic Significance of Late Jurassic Huangdi Pluton in Xiuyan, Liaodong Peninsula. Earth Science, 45(6): 2030-2043. doi: 10.3799/dqkx.2020.008

    辽东岫岩晚侏罗世荒地岩体的地球化学、年代学与Hf同位素及构造意义

    doi: 10.3799/dqkx.2020.008
    基金项目: 

    国家自然科学基金项目 41272223

    国家自然科学基金项目 41340024

    中国地质调查局项目 12120113098500

    详细信息
      作者简介:

      薛吉祥(1994-), 男, 硕士研究生, 构造地质学专业

      通讯作者:

      刘正宏

    • 中图分类号: P581;P597

    Geochemistry, Geochronology, Hf Isotope and Tectonic Significance of Late Jurassic Huangdi Pluton in Xiuyan, Liaodong Peninsula

    • 摘要: 辽东半岛中生代晚侏罗世岩浆活动较少,研究程度较低.通过对辽宁岫岩县荒地花岗岩岩体进行锆石U-Pb测年、岩石地球化学和锆石Lu-Hf同位素分析来进一步了解辽东半岛晚侏罗世的构造动力学背景,荒地花岗岩的岩浆锆石U-Pb加权平均年龄为161.1±3.6 Ma(MSWD=1.4),表明荒地岩体的形成时代为晚侏罗世,为燕山期岩浆活动的产物.该岩体含白云母等富铝矿物,地球化学数据也显示,该岩体为过铝质高钾钙碱性系列,富集K、Rb、Cs、Ba等大离子亲石元素,亏损Nb、Ti、P等高场强元素,具轻稀土元素富集,重稀土元素亏损的特征,Eu为中等负异常(δEu=0.33~0.80).该花岗岩A/CNK平均值为1.10,CIPW标准矿物中出现刚玉分子(>1%).由此认为该岩体为经历了高程度的结晶分异作用的S型花岗岩.荒地花岗岩CaO/Na2O比值小于0.3,εHft)小于0(-36.968~-23.298),表明该岩石由地壳的泥质岩熔融形成.两阶段Hf模式年龄TDMC=2 680~3 568 Ma,表明该岩体源岩的组成物质从地幔储库中脱离的时间为新太古代至古太古代,同时与辽东半岛侏罗纪其他花岗岩进行了比较.综上所述,该岩体形成于古太平洋板块向欧亚大陆俯冲后俯冲角度变大、向更深处俯冲的背景之下.

       

    • 图  1  大地构造位置图(a)和辽东半岛中生代岩浆岩分布图(b)

      图a据赵国春(2009);图b据Wu et al.(2005)

      Fig.  1.  Geological regional location map of study area (a) and distribution of Mesozoic intrusions in the Liaodong Peninsula(b)

      图  2  辽东半岛岫岩县荒地地区地质简图

      1.第四纪;2.小岭组;3.小东沟组;4.温家沟组;5.锉草沟组;6.二长花岗岩;7.似斑状二长花岗岩;8.二长花岗岩;9.闪长岩;10.黑云母二长花岗岩;11.伟晶岩;12.辽河群;13.韧性变形界线;14.韧性剪切带;15.推测性质不明断层;16.实测性质不明断层;17.航磁解译断层;18.构造破碎带;19.角度不整合界线;20.采样点

      Fig.  2.  Geological sketch map of Huangdi area in Xiuyan, Liaodong Peninsula

      图  3  荒地花岗岩镜下照片

      a.B3088⁃1;b.B4028⁃1;c.B6005⁃1;d.DYN⁃1;荒地花岗岩手标本照片e和f.Pl.斜长石;Qz.石英;Mi.微斜长石;Bit.黑云母;Mu.白云母

      Fig.  3.  Microscope photograghs for Huangdi granite rocks

      图  4  辽东半岛荒地花岗岩的SiO2⁃K2O图解(a)和A/CNK⁃A/NK图解(b)

      图a据Peccerillo and Taylor (1976);b据Shand(1943)

      Fig.  4.  Plots of SiO2⁃K2O (a) and A/CNK⁃A/NK (b) for Huangdi granites, Liaodong Peninsula

      图  5  球粒陨石标准化稀土元素配分曲线(a)和辽东半岛荒地花岗岩的原始地幔标准化微量元素蛛网图(b)

      球粒陨石值据Boynton(1984);原始地幔值据Sun and McDonough(1989)

      Fig.  5.  Chondrite⁃normalized REE patterns (a) and primitive mantle⁃normalized trace element patterns of the granite from the Huangdi pluton in Xiuyan, Liaodong Peninsula (b)

      图  6  辽东半岛荒地花岗岩部分锆石阴极发光图像

      实线圆圈代表锆石U⁃Pb测试位置;虚线圆圈代表锆石Hf同位素测试位置

      Fig.  6.  CL images of representative zircons from Huangdi granites in Liaodong Peninsula

      图  7  辽东半岛荒地锆石U⁃Pb协和年龄图

      Fig.  7.  SHRIMP U⁃Pb concordia diagram of zircons of the granites from Huangdi pluton in Xiuyan, Liaodong Peninsula

      图  8  荒地花岗岩锆石的TεHf(t)图解

      Fig.  8.  TεHf(t) plot for the zircons of Huangdi granite

      图  9  Sr/Y⁃Y图解(a)和(La/Yb)N⁃YbN图解(b)

      Fig.  9.  Sr/Y⁃Y (a) and (La/Yb)N⁃YbN (b) diagrams of the Huangdi granite in Xiuyan, Liaodong Peninsula

      图  10  Rb⁃(Y+Nb)图解(a)、Nb⁃Y图解(b)、Rb⁃(Ta+Yb)图解(c)

      syn⁃COLG为同碰撞花岗岩,VAG为火山弧花岗岩,WPG为板内花岗岩,ORG为洋中脊花岗岩;据Pearce et al. (1984)

      Fig.  10.  Rb⁃Y+Nb diagram(a), Nb⁃Y diagram(b), Rb⁃Ta+Yb diagram(c) of Huangdi granite in Xiuyan, Liaodong Peninsula

      表  1  荒地花岗岩的主量元素(%)和微量元素(10-6)分析结果

      Table  1.   Major (%) and trace (10-6) element concentrations of the granite rocks from Huangdi area

      DYN⁃1 B4028⁃1 B6005⁃1 B3088⁃1
      SiO2 73.6 73.9 74.6 73.7
      TiO2 0.11 0.09 0.11 0.14
      Al2O3 14.40 14.30 13.85 14.35
      Fe2O3 1.03 1.06 1.42 1.39
      MnO 0.02 0.02 0.03 0.03
      MgO 0.17 0.15 0.17 0.27
      CaO 1.24 0.70 0.89 1.18
      Na2O 3.98 3.97 3.76 4.01
      K2O 4.08 4.66 4.45 3.89
      P2O5 0.03 0.03 0.03 0.03
      FeOT 0.93 0.95 1.28 1.25
      Total 98.66 98.88 99.31 98.99
      K2O/Na2O 1.03 1.17 1.18 0.97
      K2O+Na2O 8.06 8.63 8.21 7.90
      A/CNK 1.09 1.11 1.10 1.11
      A/NK 1.31 1.24 1.26 1.33
      Ba 851 576 909 1350
      Rb 144.0 211 209 138.5
      Sr 378 206 289 495
      Zr 75 65 100 134
      Nb 8.1 13.4 17.4 10.1
      Cr 20 30 30 40
      La 26.3 26.8 45.7 46.8
      Ce 48.4 51.7 85.9 86.4
      Pr 4.98 5.05 8.21 7.76
      Nd 16.7 17.9 27.9 26.2
      Sm 2.73 3.26 4.66 4.22
      Eu 0.58 0.39 0.46 0.98
      Gd 2.01 2.64 3.64 2.98
      Tb 0.33 0.39 0.63 0.49
      Dy 1.94 2.02 3.57 2.58
      Ho 0.40 0.36 0.73 0.54
      Er 1.26 1.18 2.46 1.78
      Tm 0.17 0.18 0.34 0.24
      Yb 1.12 1.12 2.45 1.62
      Lu 0.13 0.14 0.35 0.24
      Y 12.3 11.8 24.8 16.8
      Cs 1.00 1.10 2.31 0.75
      Ta 0.7 0.9 1.7 1.0
      Hf 2.0 2.2 3.4 3.5
      ΣREE 107.05 113.13 187 182.83
      LREE 99.69 105.1 172.83 172.36
      HREE 7.36 8.03 14.17 10.47
      LREE/HREE 13.54 13.09 12.20 16.46
      (La/Yb)N 15.83 16.13 12.58 19.48
      δEu 0.73 0.39 0.33 0.80
      Rb/Sr 0.38 1.02 0.72 0.28
      Nb/Ta 11.57 14.89 10.24 10.10
      CaO/Na2O 0.31 0.18 0.24 0.29
      Rb/Sr 0.38 1.02 0.72 0.28
      Rb/Ba 0.17 0.37 0.23 0.10
      Rb/Nb 17.78 15.75 12.01 13.71
      Zr/Hf 37.5 29.5 29.4 38.3
      Sr/Ba 1.51 1.31 1.29 1.63
      DI 89.69 92.15 90.54 88.69
      刚玉 1.26 1.53 1.29 1.47
      下载: 导出CSV

      表  2  荒地白云母二长花岗岩的LA⁃MC⁃ICP⁃MS锆石U⁃Pb分析结果

      Table  2.   LA⁃MC⁃ICP⁃MS zircon U⁃Pb data of the muscovite monzogranite from Huangdi pluton in Xiuyan, Liaodong Peninsula

      测点号 元素含量(×10-6) Th/
      U
      同位素比值 同位素年龄(Ma)
      Pb Th U 207Pb/
      206Pb
      207Pb/
      235U
      206Pb/
      238U
      207Pb/
      206Pb
      207Pb/
      235U
      206Pb/
      238U
      DYN⁃1⁃1 25.7 82.9 1 026 0.08 0.050 3 0.002 4 0.170 0.007 0.024 8 0.000 5 209 109 159 6 158 3
      DYN⁃1⁃2 171.8 182.1 487 0.37 0.116 8 0.002 2 4.957 0.093 0.307 5 0.003 7 1 907 33 1 812 16 1 728 18
      DYN⁃1⁃3 6.9 72.4 198 0.37 0.045 8 0.009 1 0.217 0.048 0.032 8 0.002 0 191 29 200 40 208 12
      DYN⁃1⁃5 26.6 100.5 1 044 0.10 0.050 5 0.001 8 0.173 0.006 0.024 9 0.000 4 220 51 162 5 159 2
      DYN⁃1⁃8 87.1 52.7 254 0.21 0.135 2 0.008 8 5.800 0.372 0.309 8 0.007 3 2 166 113 1 946 56 1 740 36
      DYN⁃1⁃9 57.5 163.3 2 227 0.07 0.049 8 0.001 2 0.177 0.005 0.025 8 0.000 4 187 57 165 4 164 3
      DYN⁃1⁃10 3.7 81.4 130 0.62 0.053 3 0.006 8 0.169 0.022 0.023 9 0.000 9 339 294 158 19 152 6
      DYN⁃1⁃11 95.7 105.1 351 0.30 0.113 9 0.002 1 3.723 0.069 0.237 2 0.003 0 1 863 33 1 576 15 1 372 16
      DYN⁃1⁃14 89.5 162.5 251 0.65 0.117 0 0.002 2 4.700 0.092 0.290 9 0.003 1 1 922 35 1 767 16 1 646 15
      DYN⁃1⁃18 40.3 251.4 1 470 0.17 0.051 4 0.001 9 0.182 0.007 0.025 7 0.000 3 261 85 170 6 164 2
      DYN⁃1⁃19 6.7 188.5 213 0.89 0.059 4 0.010 5 0.177 0.028 0.025 4 0.001 2 583 391 166 25 162 7
      下载: 导出CSV

      表  3  辽东荒地花岗岩的Hf同位素分析结果

      Table  3.   Hf isotope analysis results of Huangdi granite in Liaodong Peninsula

      测点号 T(Ma) 176Hf/177Hf 176Lu/177Hf 176Yb/177Hf εHf(t) TDMHf(Ma) TDMC(Ma)
      DYN⁃1⁃01 158 0.282 018 0.000 81 0.040 30 3.0 -23.298 074 07 1 728 2 680
      DYN⁃1⁃02 1 907 0.281 662 0.001 67 0.081 59 33.0 1.181 794 147 2 266 2 471
      DYN⁃1⁃03 208 0.281 602 0.001 01 0.049 04 12.4 -36.968 833 13 2 311 3 568
      DYN⁃1⁃04 159 0.281 807 0.000 68 0.029 45 2.4 -30.711 580 41 2 010 3 144
      DYN⁃1⁃05 2 166 0.281 919 0.000 73 0.034 03 113.0 17.334 503 65 1 859 1 672
      DYN⁃1⁃06 164 0.281 960 0.002 63 0.139 92 2.7 -25.411 689 43 1 898 2814
      DYN⁃1⁃07 152 0.281 918 0.000 81 0.039 43 5.5 -26.957 914 33 1 866 2 904
      DYN⁃1⁃08 1922 0.281 556 0.001 12 0.052 44 34.7 -1.557 603 622 2 380 2 652
      DYN⁃1⁃09 162 0.281 929 0.001 78 0.086 19 7.4 -26.460 603 56 1 898 2 879
      下载: 导出CSV
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    • 收稿日期:  2019-11-02
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