新疆西凤山金矿床q6含金石英脉原生晕特征

高雅宁, 杨兴科, 张康, 何虎军, 张晓龙, 孙继东. 新疆西凤山金矿床q6含金石英脉原生晕特征[J]. 西北地质, 2016, 49(2): 124-133.
引用本文: 高雅宁, 杨兴科, 张康, 何虎军, 张晓龙, 孙继东. 新疆西凤山金矿床q6含金石英脉原生晕特征[J]. 西北地质, 2016, 49(2): 124-133.
GAO Yaning, YANG Xingke, ZHANG Kang, HE Hujun, ZHANG Xiaolong, SUN Jidong. Study on Primary Halo Characteristics of q6 Gold-bearing Quartz Veinsin Xifengshan Gold Deposit, Xinjiang[J]. Northwestern Geology, 2016, 49(2): 124-133.
Citation: GAO Yaning, YANG Xingke, ZHANG Kang, HE Hujun, ZHANG Xiaolong, SUN Jidong. Study on Primary Halo Characteristics of q6 Gold-bearing Quartz Veinsin Xifengshan Gold Deposit, Xinjiang[J]. Northwestern Geology, 2016, 49(2): 124-133.

新疆西凤山金矿床q6含金石英脉原生晕特征

  • 基金项目: 中国地质调查局地质调查工作"新疆北部晚古生代大规模岩浆作用与成矿耦合关系研究"(1212011121092)

Study on Primary Halo Characteristics of q6 Gold-bearing Quartz Veinsin Xifengshan Gold Deposit, Xinjiang

  • 在调研西凤山金矿床地质特征的基础上,选择有代表性的q6含金石英脉进行原生晕地球化学测量和异常建模评价工作。对该含金石英脉10项元素的测试分析结果表明:地表Au原生晕强度大于钻孔和坑道Au原生晕强度;q6主矿脉地表原生晕Au2极度清晰,且达到矿体原生晕规模;q6矿脉地表原生晕横向分带总体呈对称分布,并指示了矿体具有向北陡倾的趋势,横向分带序列显示出主成矿元素具异常高强度与较大线规模等特点。该主矿脉中元素的分布及变化规律的研究,对该矿区进一步的矿体追索与工程布置具有指导意义。
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出版历程
收稿日期:  2015-07-23
修回日期:  2016-02-20
刊出日期:  2016-06-15

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