黔西南水银洞爆破角砾岩筒与金元素超常富集

邱小平, 刘世川, 魏密. 2021. 黔西南水银洞爆破角砾岩筒与金元素超常富集[J]. 地球学报, (6): 849-858. doi: 10.3975/cagsb.2021.101901
引用本文: 邱小平, 刘世川, 魏密. 2021. 黔西南水银洞爆破角砾岩筒与金元素超常富集[J]. 地球学报, (6): 849-858. doi: 10.3975/cagsb.2021.101901
QIU Xiao-ping, LIU Shi-chuan, WEI Mi. 2021. Fluid Explosion Breccia Pipe and Gold Supernormal Enrichment in Shuiyindong Gold Ore Deposit, Southwest Guizhou Province. Acta Geoscientica Sinica, (6): 849-858. doi: 10.3975/cagsb.2021.101901
Citation: QIU Xiao-ping, LIU Shi-chuan, WEI Mi. 2021. Fluid Explosion Breccia Pipe and Gold Supernormal Enrichment in Shuiyindong Gold Ore Deposit, Southwest Guizhou Province. Acta Geoscientica Sinica, (6): 849-858. doi: 10.3975/cagsb.2021.101901

黔西南水银洞爆破角砾岩筒与金元素超常富集

  • 基金项目:

    本文由国家自然科学基金项目(编号: 41172075)资助

详细信息
    作者简介: 邱小平, 男, 1959年生。博士, 研究员, 博士生导师。长期从事动力成岩成矿与碰撞造山带成矿研究, 近年来重点探讨滇黔桂“金三角”金矿床成矿动力学问题。通讯地址: 100037, 北京市西城区百万庄大街26号。E-mail: qiuxping@cags.ac.cn
  • 中图分类号: P618.51

Fluid Explosion Breccia Pipe and Gold Supernormal Enrichment in Shuiyindong Gold Ore Deposit, Southwest Guizhou Province

  • 水银洞金矿床曾被认为是滇黔桂地区最有代表性的微细浸染型金矿(卡林型金矿), 然而矿床的金品位明显高于一般意义上的卡林型金矿床, 且金矿体与气液爆破角砾岩关系密切。气液爆破角砾岩呈垂直筒状产状, 两侧断裂矿化带呈向上扩张的“喇叭口”状成矿空间, 富金矿体紧密围绕角砾岩筒分布。根据野外和显微镜观察, 角砾岩块成分复杂与显著磨圆。气液角砾岩筒的角砾岩显著富集金、稀土、亲地幔过渡元素Ti、Cr、Ni、Co、V等, 以及Zr、Hf等, 明显地区别于围岩, 反映出深源流体快速上升的气液爆破角砾岩的特征, 角砾岩筒实际上具备含金成矿流体的上涌通道的功能。岩筒中早期角砾岩的角砾含 Au达18×10–6, 属于深部金矿体的爆破碎块, 显示出水银洞金矿床可观的深部找矿勘探前景。
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收稿日期:  2021-06-21
修回日期:  2021-10-14

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