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    广东文光岭铅锌铜多金属矿花岗闪长岩LA-ICP-MS锆石U-Pb定年、地球化学特征及其成因

    欧阳志侠 楚克磊 陈友良 吴晓东 杨胜虎 汪汝澎 刘东宏 汪礼明

    欧阳志侠, 楚克磊, 陈友良, 吴晓东, 杨胜虎, 汪汝澎, 刘东宏, 汪礼明, 2019. 广东文光岭铅锌铜多金属矿花岗闪长岩LA-ICP-MS锆石U-Pb定年、地球化学特征及其成因. 地球科学, 44(4): 1327-1337. doi: 10.3799/dqkx.2017.591
    引用本文: 欧阳志侠, 楚克磊, 陈友良, 吴晓东, 杨胜虎, 汪汝澎, 刘东宏, 汪礼明, 2019. 广东文光岭铅锌铜多金属矿花岗闪长岩LA-ICP-MS锆石U-Pb定年、地球化学特征及其成因. 地球科学, 44(4): 1327-1337. doi: 10.3799/dqkx.2017.591
    Ouyang Zhixia, Chu Kelei, Chen Youliang, Wu Xiaodong, Yang Shenghu, Wang Rupeng, Liu Donghong, Wang Liming, 2019. Zircon U-Pb Dating, Geochemistry and Petrogenesis of Granodiorite from Wenguangling Pb-Zn-Cu Polymetallic Deposit in Guangdong Province. Earth Science, 44(4): 1327-1337. doi: 10.3799/dqkx.2017.591
    Citation: Ouyang Zhixia, Chu Kelei, Chen Youliang, Wu Xiaodong, Yang Shenghu, Wang Rupeng, Liu Donghong, Wang Liming, 2019. Zircon U-Pb Dating, Geochemistry and Petrogenesis of Granodiorite from Wenguangling Pb-Zn-Cu Polymetallic Deposit in Guangdong Province. Earth Science, 44(4): 1327-1337. doi: 10.3799/dqkx.2017.591

    广东文光岭铅锌铜多金属矿花岗闪长岩LA-ICP-MS锆石U-Pb定年、地球化学特征及其成因

    doi: 10.3799/dqkx.2017.591
    基金项目: 

    中国地质调查局地质调查工作项目 12120114015801

    中国地质调查局地质调查工作项目 1212011120826

    详细信息
      作者简介:

      欧阳志侠(1984-), 男, 硕士, 高级工程师, 主要从事区域地质调查与矿产勘查等工作

      通讯作者:

      陈友良

    • 中图分类号: P581;P597

    Zircon U-Pb Dating, Geochemistry and Petrogenesis of Granodiorite from Wenguangling Pb-Zn-Cu Polymetallic Deposit in Guangdong Province

    • 摘要: 广东省文光岭矿床是云开地区近年来新发现的铅锌铜多金属矿.以文光岭花岗闪长岩作为研究对象,对其开展了LA-ICP-MS锆石U-Pb同位素定年和地球化学特征研究.获得其锆石206Pb/238U同位素加权平均年龄为165.7±1.9 Ma(n=18,MSWD=3.1).花岗闪长岩属于准铝质Ⅰ型花岗岩,SiO2含量在64.11%~66.64%之间,Al2O3含量为14.9%~15.57%,MgO含量在1.39%~1.61%之间,K2O+Na2O含量介于6.5%~7.21%,K2O/Na2O=1.25~2.74,铝饱和指数A/CNK=0.93~1.11.轻、重稀土元素分馏作用明显,(La/Yb)N=13.03~17.83,具有弱的负铕异常(δEu为0.70~0.88),HFSE和LILE分异明显,富集Rb、Th、U、K等元素,亏损Nb、Ta、P和Ti等元素.结合区内已有资料,认为文光岭铅锌铜多金属矿床的形成与古太平洋板块的俯冲作用密切相关.

       

    • 图  1  云开地区地质、矿产略图

      改自毛景文等(2011)楚克磊(2013)

      Fig.  1.  Geological and mineral sketch map of the Yunkai area

      图  2  广东省文光岭花岗闪长岩野外照片

      Fig.  2.  Field photos of the Wenguangling granodiorites in Guangdong Province

      图  3  广东省文光岭花岗闪长岩体LA-ICP-MS锆石U-Pb谐和图和206Pb/238U年龄谱图

      Fig.  3.  Zircon U-Pb concordia diagram and 206Pb/238U age spectra for the Wenguangling granodiorite in Guangdong Province

      图  4  广东省文光岭花岗闪长岩体的SiO2-K2O图解(a)及A/CNK-A/NK图解(b)

      Rickwood(1989)Peccerillo and Taylor(1976)

      Fig.  4.  SiO2 versus K2O (a) and A/CNK versus A/NK (b) plots for the Wenguangling granodiorites in Guangdong Province

      图  5  广东省文光岭花岗闪长岩体微量元素原始地幔标准化蛛网图(a)及稀土元素球粒陨石标准化配分曲线图(b)

      Sun and McDonough (1989)

      Fig.  5.  Primitive mantle-normalized trace element patterns (a) and chondrite-normalized REE patterns (b) diagrams of the Wenguangling granodiorites in Guangdong Province

      图  6  广东省文光岭花岗闪长岩构造环境判别图

      Syn-COLG.同碰撞花岗岩;WPG.板内花岗岩;VAG.岛弧花岗岩;ORG.洋中脊花岗岩.底图据Pearce et al.(1984)

      Fig.  6.  Tectonic setting discrimination diagram of Wenguangling granodiorites in Guangdong Province

      表  1  广东省文光岭花岗闪长岩体的主量(%)、微量和稀土元素(10-6)组成

      Table  1.   Major (%), trace (10-6) elements and REE (10-6) compositions of the Wenguangling granodiorite in Guangdong Province

      样品 YGL-01 YGL-02 HB-01 HB-02
      SiO2 66.25 64.11 66.28 66.64
      TiO2 0.46 0.50 0.55 0.50
      Al2O3 15.42 15.57 14.90 14.94
      Fe2O3 4.13 3.85 4.77 4.35
      MnO 0.10 0.24 0.11 0.08
      MgO 1.41 1.39 1.61 1.42
      CaO 2.51 3.51 3.97 3.75
      Na2O 2.94 1.93 2.89 2.96
      K2O 4.15 5.28 3.61 4.03
      P2O5 0.14 0.18 0.18 0.17
      LOI 1.84 2.61 0.96 0.56
      Total 99.43 99.25 99.90 99.48
      Be 2.2 3.0 2.3 2.1
      Sc 7 8 7 7
      V 73 81 83 77
      Cr 23 32 24 21
      Co 8 8 8 8
      Ni 4 5 5 5
      Cu < 1 4 < 1 1
      Zn 37 73 46 34
      Ga 19.0 17.7 18.6 17.7
      As 5 6 9 9
      Rb 218 351 187 202
      Ba 613 656 521 627
      Nb 10.5 10.8 12.5 11.1
      Sr 420 292 468 453
      Zr 155 151 173 140
      Hf 4.4 4.2 5.1 3.9
      Ti 2 757.7 2 997.5 3 297.3 2 997.5
      La 46.1 52.7 46.9 40.5
      Ce 66.4 83.3 79.2 69.3
      Pr 7.08 8.67 8.34 7.45
      Nd 24.3 29.2 29.3 25.3
      Sm 4.40 5.13 5.51 4.82
      Eu 1.23 1.14 1.29 1.24
      Gd 3.94 4.63 4.51 3.76
      Tb 0.58 0.69 0.72 0.58
      Dy 3.49 3.82 3.96 3.31
      Ho 0.65 0.78 0.74 0.75
      Er 1.99 2.07 2.34 1.96
      Tm 0.31 0.29 0.35 0.31
      Yb 2.16 2.12 2.55 2.23
      Lu 0.32 0.32 0.36 0.29
      Y 17.5 20.9 21.4 19.6
      K 34 450.4 43 830.9 29 967.7 33 454.2
      Ta 0.9 1.0 1.1 0.9
      P 611.04 785.63 785.63 741.98
      Th 30 30 30 30
      U 7.35 9.55 12.55 7.81
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