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    西藏岗穷拉石英脉型钼铜矿床辉钼矿Re-Os同位素定年及其地质意义

    董随亮 张志 李光明 张林奎 黄勇 付建刚 方明

    董随亮, 张志, 李光明, 张林奎, 黄勇, 付建刚, 方明, 2019. 西藏岗穷拉石英脉型钼铜矿床辉钼矿Re-Os同位素定年及其地质意义. 地球科学, 44(7): 2265-2274. doi: 10.3799/dqkx.2019.099
    引用本文: 董随亮, 张志, 李光明, 张林奎, 黄勇, 付建刚, 方明, 2019. 西藏岗穷拉石英脉型钼铜矿床辉钼矿Re-Os同位素定年及其地质意义. 地球科学, 44(7): 2265-2274. doi: 10.3799/dqkx.2019.099
    Dong Suiliang, Zhang Zhi, Li Guangming, Zhang Linkui, Huang Yong, Fu Jiangang, Fang Ming, 2019. Re-Os Dating of Molybdenite from Gangqiongla Quartz-Vein Type Mo-Cu Deposit in Tibet and Its Geological Significance. Earth Science, 44(7): 2265-2274. doi: 10.3799/dqkx.2019.099
    Citation: Dong Suiliang, Zhang Zhi, Li Guangming, Zhang Linkui, Huang Yong, Fu Jiangang, Fang Ming, 2019. Re-Os Dating of Molybdenite from Gangqiongla Quartz-Vein Type Mo-Cu Deposit in Tibet and Its Geological Significance. Earth Science, 44(7): 2265-2274. doi: 10.3799/dqkx.2019.099

    西藏岗穷拉石英脉型钼铜矿床辉钼矿Re-Os同位素定年及其地质意义

    doi: 10.3799/dqkx.2019.099
    基金项目: 

    中国地质调查局地质调查项目 DD20190147

    国家自然科学基金 41702080

    国家重点研发计划深地资源开采项目 2016YFC0600308

    详细信息
      作者简介:

      董随亮(1983-), 男, 工程师, 从事青藏高原地质研究工作

      通讯作者:

      张志

    • 中图分类号: P581

    Re-Os Dating of Molybdenite from Gangqiongla Quartz-Vein Type Mo-Cu Deposit in Tibet and Its Geological Significance

    • 摘要: 西藏岗穷拉钼铜矿床是近年在冈底斯带东段新发现的石英脉型钼铜矿.本次研究对岗穷拉矿床8件石英-辉钼矿脉样品中辉钼矿进行Re-Os同位素精确定年.测试结果表明,辉钼矿的模式年龄加权平均值为22.6±0.2 Ma(MSWD=1.3),等时线年龄为24.1±1.3 Ma(MSWD=1.1),二者在误差范围内基本一致,代表了岗穷拉矿床的成矿年龄,该年龄明显早于区域上南冈底斯带斑岩型钼铜矿的成矿时代(集中在17~12 Ma).辉钼矿中Re含量在239.1×10-6~314.7×10-6之间,指示成矿物质可能主要为幔源.结合区域上渐新世-早中新世大规模成矿作用的资料,岗穷拉钼铜矿可能为印度大陆与欧亚大陆碰撞造山过程中晚碰撞与后碰撞转换阶段成矿作用的产物.

       

    • 图  1  冈底斯成矿带地质简图与主要矿产分布图(a)及岗穷拉矿床地质图(b)

      Zheng et al.(2015)修编

      Fig.  1.  Geological map of Gangdise metallogenic belt and distribution map of major minerals (a) and geological map of Gangqiongla deposit (b)

      图  2  岗穷拉矿区辉钼矿特征

      a~c.石英脉中辉钼矿;d, e.石英脉中辉钼矿镜下照片;f.含辉钼矿石英脉中黄铜矿;Mo.辉钼矿;Cp.黄铜矿

      Fig.  2.  Characteristics of molybdenite in Gangqiongla deposit

      图  3  岗穷拉矿区辉钼矿Re-Os等时线年龄(a)及加权平均年龄图解(b)

      Fig.  3.  Re-Os isochron (a) and weighted average of model age (b) of molybdenites from Gangqiongla deposit

      表  1  岗穷拉矿床辉钼矿Re-Os同位素测年结果

      Table  1.   Re-Os isotopic data of molybdenites from Gangqiongla deposit

      样品
      编号
      样重
      (g)
      Re(10-6) 普Os(10-9) 187Re(10-6) 187Os(10-9) 模式年龄(Ma)
      测定值 1σ 测定值 1σ 测定值 1σ 测定值 1σ 测定值 1σ
      JC07 0.010 97 245.9 2.2 0.064 7 0.047 3 154.5 1.4 57.51 0.59 22.33 0.35
      JC08 0.010 20 239.1 2.3 0.008 9 0.034 1 150.3 1.4 55.81 0.45 22.28 0.33
      JC09 0.010 51 278.1 3.1 0.018 3 0.088 7 174.8 1.9 66.37 0.92 22.79 0.44
      JC10 0.010 55 249.7 2.0 0.008 5 0.032 6 156.9 1.2 59.49 0.50 22.75 0.32
      JC11 0.010 45 314.7 3.2 0.113 0 0.140 0 197.8 2.0 75.19 0.76 22.81 0.37
      JC12 0.010 87 292.9 2.4 0.019 4 0.064 9 184.1 1.5 69.56 0.64 22.68 0.33
      JC13 0.010 18 271.0 2.4 0.017 7 0.110 4 170.3 1.5 63.94 0.64 22.53 0.35
      JC14 0.011 27 267.5 2.6 0.033 1 0.023 6 168.2 1.6 63.19 0.59 22.55 0.35
      注:辉钼矿模式年龄t计算方法为:t=λ-1ln(1+187Os/187Re),λ187Re的衰变常数1.666×10-11 a-1(±1.02%);测试报告编号(QTNL2013052).
      下载: 导出CSV

      表  2  冈底斯成矿带主要矿床成岩与成矿时代表

      Table  2.   The dating result of deposits in Gangdise metallogenic belt

      序号 矿区 矿种 岩矿石 测年方法 年龄(Ma) 成矿环境 资料来源
      1 雄村 铜金矿 辉钼矿 Re-Os 173 俯冲期 唐菊兴等,2010
      2 龙根 铅锌矿 花岗斑岩 锆石U-Pb 61.4 主碰撞 段志明等,2014
      3 查格勒 铅锌矿 花岗斑岩 锆石U-Pb 63.2 主碰撞 黄瀚霄等,2012
      4 斯弄多 铅锌矿 云母 Ar-Ar 61-63 主碰撞 Li et a.,2019
      5 拿若松多 铅锌矿 花岗斑岩 锆石U-Pb 62.5 主碰撞 Ji et al., 2014
      6 新嘎果 铅锌矿 黑云母花岗岩 锆石U-Pb 56.5 主碰撞 Wang et al., 2016
      7 勒青拉 铅锌矿 花岗闪长斑岩 锆石U-Pb 60.8 主碰撞 Wang et al., 2016
      8 龙马拉 铅锌矿 黑云二长岩 锆石U-Pb 55.7 主碰撞 Wang et al., 2015b
      9 蒙亚啊 铅锌矿 辉钼矿 Re-Os 63.6 主碰撞 Wang et al., 2015b
      10 列廷冈 铅锌矿 辉钼矿 Re-Os 62.3 主碰撞 杨毅等,2014
      11 亚圭拉 铅锌矿 石英斑岩 锆石U-Pb 62.4 主碰撞 黄克贤等,2012
      12 明则 钼矿 辉钼矿 Re-Os 30.3 晚碰撞 闫学义等,2010
      13 努日 钨铜矿 辉钼矿 Re-Os 23.6 晚碰撞 闫学义等,2010
      14 冲木达 铜金矿 花岗岩 锆石U-Pb 27.7 晚碰撞 莫济海等,2008
      15 汤不拉 铜矿 辉钼矿 Re-Os 20.9 后碰撞 王保弟等,2010
      16 鸡公村 钼矿 辉钼矿 Re-Os 21.8 后碰撞 张苏坤等,2013
      17 甲玛 铜多金属矿 辉钼矿 Re-Os 15.3 后碰撞 Ying et al., 2014
      18 驱龙 铜多金属矿 辉钼矿 Re-Os 16.4 后碰撞 孟祥金等,2003
      19 拉抗俄 铜钼矿 辉钼矿 Re-Os 13.1 后碰撞 Leng et al., 2016
      20 冲江 铜钼矿 辉钼矿 Re-Os 14.8 后碰撞 郑有业等,2004
      下载: 导出CSV
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