地球化学勘查在早子沟金矿中的应用及启示

    Application and enlightenment of the geochemical exploration in Zaozigou gold deposit

    • 摘要: 早子沟金矿位于西秦岭造山带的西北部,植被发育,基岩出露较差,地球化学勘查是区域最有效的勘查方法之一。在系统梳理早子沟金矿1:20万、1:5万水系沉积物测量及1:1万土壤测量地球化学特征的基础上,结合深部钻孔SK8314原生晕特征,发现Au元素与Sb、As、Hg、Ag、Cu等元素具有正相关性,特别是Au、Sb元素组合是金矿找矿的直接地球化学标志,深部原生晕分带序列为Bi-Cu-Mo-Sb-Ag-Au-W-As-Sn-Zn-Cd-Pb-Cr-Ni-Co-Hg,尾晕元素Bi和近矿晕元素Cu位于分带序列前缘晕,Pb、Zn元素位于分带序列尾晕,表明矿体具有多期成矿叠加特征,深部可能存在盲矿体。同时在钻孔SK8314孔深1 850 m以下,随着深度增大,地球化学参数(As+Sb)/(Bi+Mo)值和100·Sb/(Bi·Mo)值呈现逐渐增大的趋势,指示深部可能存在盲矿体,依然具有较大的找矿空间。研究成果可为早子沟金矿的深部及外围找矿提供参考。

       

      Abstract: Zaozigou gold deposit is located in the northwest of West Qinling orogenic belt, with well-developed vegetation and poor bedrock outcropping. The geochemical exploration is one of the most effective exploration methods in the region. On the basis of systematically combing the geochemical characteristics of 1:200,000 and 1:50,000 water sediment measurements and 1:10,000 soil measurements of Zaozigou gold deposit, the authors found that Au has a positive correlation with Sb, As, Hg, Ag and Cu, combined with the characteristics of the primary halo of the deep borehole SK8314. Especially, the combination of Au and Sb is a direct geochemical marker for gold prospecting. The deep primary halo zoning sequence is Bi-Cu-Mo-Sb-Ag-Au-W-As-Sn-Zn-Cd-Pb-Cr-Ni-Co-Hg, and Bi is located in the leading halo of the zoning sequence. Cu is located in the leading halo of the zoning sequence, and Pb and Zn are located in the tail halo of the zoning sequence, indicating that the ore body has the characteristics of multi-stage metallogenic superposition, probably with blind ore body in the depth. At the same time, the ratios of geochemical parameters (As+Sb)/(Bi+Mo) and 100·Sb/(Bi·Mo) gradually increased with the increasing depth at hole SK8314 below 1 850 m, indicating blind ore bodies in the deeper part and a large prospecting space. The research results could provide some references for deep and peripheral prospecting in Zaozigou.

       

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