李存有, 施立达. 张全庄金矿元素地球化学特征及找矿意义[J]. 地质与资源, 1999, 8(4): 223-228. DOI: 10.13686/j.cnki.dzyzy.1999.04.005
    引用本文: 李存有, 施立达. 张全庄金矿元素地球化学特征及找矿意义[J]. 地质与资源, 1999, 8(4): 223-228. DOI: 10.13686/j.cnki.dzyzy.1999.04.005
    LI Cun-you, SHI Li-da. THE ELEMENTAL GEOCHEMISTRY AND EXPLORING SIGNIFICANCE OF ZHANGQUANZHUANG GOLD DEPOSIT[J]. Geology and Resources, 1999, 8(4): 223-228. DOI: 10.13686/j.cnki.dzyzy.1999.04.005
    Citation: LI Cun-you, SHI Li-da. THE ELEMENTAL GEOCHEMISTRY AND EXPLORING SIGNIFICANCE OF ZHANGQUANZHUANG GOLD DEPOSIT[J]. Geology and Resources, 1999, 8(4): 223-228. DOI: 10.13686/j.cnki.dzyzy.1999.04.005

    张全庄金矿元素地球化学特征及找矿意义

    THE ELEMENTAL GEOCHEMISTRY AND EXPLORING SIGNIFICANCE OF ZHANGQUANZHUANG GOLD DEPOSIT

    • 摘要: 张全庄金矿是河北省一危机矿山.矿山多为采空区,矿脉中硫化物分布不均匀.矿脉的不同围岩为统一的元素地球化学整体.通过采取与矿脉等距近矿蚀变岩,研究这些蚀变岩中元素的带入带出特征,分析成矿规律,建立了张全庄金矿矿脉原生晕元素组合分带模式,即As、Sb、Ag等元素为头晕元素,Cu、Ag、Au、Pb、Zn等元素为矿中元素,Mo为尾晕元素.运用此模式对张全庄金矿进行深部成矿预测,成功地发现了新矿体.

       

      Abstract: Zhangquanzhuang gold deposit is an old gold deposit in Hebei Province,China By 1994,only a little gold was reserved. Most of gold veins have been mined. The sulfides scatter in the veins unevenly,but the various kinds of wall-rocks share the same elemental geochemistry environment. We took the altered wall-rocks which have the same distances from vein in accordance with the above facts. Some orebodies have been found by studying the elemental migration features in those altered wall-rocks and establishing a model of elemental zoning of primary dispersion halo,i.e., As,Sb and Ag are the top halo elements,Cu,Ag,Au,Pb and Zn are the mineralization elements, and Mo is the rear halo elemet.

       

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