西藏冈底斯中段错杰地区花岗斑岩年代学、地球化学特征及其找矿意义

胡林, 徐琳, 肖进, 徐刚, 罗绍强. 2021. 西藏冈底斯中段错杰地区花岗斑岩年代学、地球化学特征及其找矿意义. 中国地质调查, 8(5): 53-63. doi: 10.19388/j.zgdzdc.2021.05.07
引用本文: 胡林, 徐琳, 肖进, 徐刚, 罗绍强. 2021. 西藏冈底斯中段错杰地区花岗斑岩年代学、地球化学特征及其找矿意义. 中国地质调查, 8(5): 53-63. doi: 10.19388/j.zgdzdc.2021.05.07
HU Lin, XU Lin, XIAO Jin, XU Gang, LUO Shaoqiang. 2021. Chronology, geochemical characteristics and prospecting significance of the granite porphyry in Cuojie area of Middle Gangdise in Tibet. Geological Survey of China, 8(5): 53-63. doi: 10.19388/j.zgdzdc.2021.05.07
Citation: HU Lin, XU Lin, XIAO Jin, XU Gang, LUO Shaoqiang. 2021. Chronology, geochemical characteristics and prospecting significance of the granite porphyry in Cuojie area of Middle Gangdise in Tibet. Geological Survey of China, 8(5): 53-63. doi: 10.19388/j.zgdzdc.2021.05.07

西藏冈底斯中段错杰地区花岗斑岩年代学、地球化学特征及其找矿意义

  • 基金项目:

    中国地质调查局“西藏厅宫地区1:5万区域地质调查(编号: DD20160015)”项目资助

详细信息
    作者简介: 胡林(1986—),男,工程师,主要从事区域地质调查工作。Email: 276487709@qq.com。
    通讯作者: 徐琳(1986—),男,高级工程师,主要从事区域地质调查工作。Email: 664998491@qq.com。
  • 中图分类号: P588.13;P597.3;P595

Chronology, geochemical characteristics and prospecting significance of the granite porphyry in Cuojie area of Middle Gangdise in Tibet

More Information
  • 在西藏冈底斯中段错杰地区发现一套含孔雀石的花岗斑岩,为确定其形成时代、成因及其找矿意义,对该套花岗斑岩进行了岩相学、LA- ICP-MS锆石U-Pb年代学及地球化学特征研究。结果表明: 该套花岗斑岩中的锆石为岩浆成因,锆石206Pb/238U加权平均年龄为(13.9±0.2)Ma,侵入时代为中新世。主量元素地球化学测试结果显示花岗斑岩具有富SiO2、富Al2O3、富碱、富钠的钙碱性特征。微量元素地球化学测试结果显示花岗斑岩相对富集U、Th等大离子亲石元素,亏损Nb、Yb等高场强元素,稀土总量为(47.4~141.4)×10-6,轻稀土相对富集,具正Eu异常。经过综合分析,认为花岗斑岩形成于加厚下地壳的部分熔融,形成过程中可能发生了部分分离结晶作用。通过将花岗斑岩的地质特征与区域典型矿床进行对比,发现错杰地区花岗斑岩具有与冈底斯斑岩铜矿相似的地质特征及成矿系统,深部可能隐伏有较大的含矿斑岩体,具有较好的找矿前景。
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收稿日期:  2020-07-21
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