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赞比亚谦比西铜矿花岗岩年龄及其指示意义

刘晓阳, 王杰, 任军平, 龚鹏辉, 何胜飞, 贺福清. 2017. 赞比亚谦比西铜矿花岗岩年龄及其指示意义[J]. 中国地质, 44(4): 755-765. doi: 10.12029/gc20170408
引用本文: 刘晓阳, 王杰, 任军平, 龚鹏辉, 何胜飞, 贺福清. 2017. 赞比亚谦比西铜矿花岗岩年龄及其指示意义[J]. 中国地质, 44(4): 755-765. doi: 10.12029/gc20170408
LIU Xiaoyang, WANG Jie, REN Junping, GONG Penghui, HE Shengfei, HE Fuqing. 2017. Age of granites from the Chambishi copper mine in Zambia and its implications[J]. Geology in China, 44(4): 755-765. doi: 10.12029/gc20170408
Citation: LIU Xiaoyang, WANG Jie, REN Junping, GONG Penghui, HE Shengfei, HE Fuqing. 2017. Age of granites from the Chambishi copper mine in Zambia and its implications[J]. Geology in China, 44(4): 755-765. doi: 10.12029/gc20170408

赞比亚谦比西铜矿花岗岩年龄及其指示意义

  • 基金项目:
    中国地质调查局项目(121201006000150014)资助
详细信息
    作者简介: 刘晓阳, 男, 1977生, 高级工程师, 主要从事地质矿产勘查工作; E-mail:lxylyw2003@163.com
  • 中图分类号: P588.12+; P597+.3;P618.41

Age of granites from the Chambishi copper mine in Zambia and its implications

  • Fund Project: Supported by China Geological Survey Program (No. 121201006000150014)
More Information
    Author Bio: LIU Xiaoyang, male, born in 1977, senior geologist, engages in the study of geology and mineral resources exploration; E-mail: lxylyw2003@163.com .
  • 赞比亚谦比西铜矿位于新元古代卢菲利安弧构造带内。矿体呈似层状分布于新元古代罗安组的砂页岩中。罗安组地层不整合于古元古代穆瓦系砂砾岩之上,穆瓦系砂砾岩不整合于下部谦比西花岗岩基底之上。锆石U-Pb测年结果表明谦比西花岗岩年龄为(1984±6)Ma~(1986±6)Ma;穆瓦系年龄上限为(1932±8)Ma。谦比西花岗岩岩石地球化学、稀土元素与球粒陨石配分特征均表现为S型花岗岩的特征。区域地质资料表明,可能由于古元古代班韦卢地块与坦桑尼亚太古宙克拉通碰撞作用诱发了卢菲利安古元古代花岗岩基底的形成;太古宙刚果克拉通于早元古代(2100~1800 Ma)期间活化,并形成一稳定块体。

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  • 图 1  谦比西铜矿区域地质简图(A—大地构造位置;B—区域地质简图)

    Figure 1. 

    图 2  谦比西铜矿地质简图及取样位置

    Figure 2. 

    图 3  锆石阴极发光照片(a-样品TWPd174;b-样品TWZK17-7-01;c-样品TWZK17-7-02)

    Figure 3. 

    图 4  谦比西铜矿花岗岩锆石U-Pb谐和图

    Figure 4. 

    图 5  谦比西铜矿花岗岩地球化学图解

    Figure 5. 

    表 1  锆石U-Pb测年结果

    Table 1.  Results of U-Pb dating of zircon samples

    下载: 导出CSV

    表 2  谦比西铜矿样品全岩地球化学数据

    Table 2.  Whole rock geochemical data of samples from the Chambishi copper mine

    下载: 导出CSV
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出版历程
收稿日期:  2017-07-18
修回日期:  2017-08-10
刊出日期:  2017-08-25

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