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    张方方, 王建平, 王臣, 刘冲昊, 曹瑞荣, 程建军, 杨永荣, 齐峰, 王罗. 陕西双王金矿床轴(垂)向黄铁矿中微量元素变化规律及深部预测[J]. 中国地质, 2014, 41(5): 1650-1663.
    引用本文: 张方方, 王建平, 王臣, 刘冲昊, 曹瑞荣, 程建军, 杨永荣, 齐峰, 王罗. 陕西双王金矿床轴(垂)向黄铁矿中微量元素变化规律及深部预测[J]. 中国地质, 2014, 41(5): 1650-1663.
    ZHANG Fang-fang, WANG Jian-ping, WANG Chen, LIU Chong-hao, CAO Rui-rong, CHENG Jian-jun, YANG Yong-rong, QI Feng, WANG Luo. The vertical variation of trace elements and its applications to metallogenic prognosis in the Shuangwang gold deposit, Shaanxi Province[J]. GEOLOGY IN CHINA, 2014, 41(5): 1650-1663.
    Citation: ZHANG Fang-fang, WANG Jian-ping, WANG Chen, LIU Chong-hao, CAO Rui-rong, CHENG Jian-jun, YANG Yong-rong, QI Feng, WANG Luo. The vertical variation of trace elements and its applications to metallogenic prognosis in the Shuangwang gold deposit, Shaanxi Province[J]. GEOLOGY IN CHINA, 2014, 41(5): 1650-1663.

    陕西双王金矿床轴(垂)向黄铁矿中微量元素变化规律及深部预测

    The vertical variation of trace elements and its applications to metallogenic prognosis in the Shuangwang gold deposit, Shaanxi Province

    • 摘要: 提要:凤太矿集区是秦岭重要的铅锌金多金属成矿区之一, 双王金矿是该成矿区中典型的角砾岩型金矿床。本文采用格里戈良提出的原生晕分带指数法, 详细研究了双王金矿床KT9矿体和KT8矿体中ZK18-5、ZK30-1和ZK40-5 3个坑内钻孔的原生晕轴(垂)向分带特征, 通过各钻孔中原生晕分带指数垂向变化规律、微量元素衬值及地球化学参数分析进行深部矿化预测。结果显示, 双王金矿床原生晕轴(垂)向分带序列呈明显的反带现象, ZK18-5中在标高950 m附近矿化程度最好, 矿体向深部逐渐尖灭; ZK30-1在标高980 m附近矿化程度最好, 其深部预测有串珠状矿体存在, 深部矿化前景较好; ZK40-5在标高850 m附近矿化程度最好, 预测深部矿体仍有较大规模的延伸, 深部矿化前景较好。

       

      Abstract: Abstract: The Fengtai ore concentration area is an important Pb-Zn-Au metallogenic area in the Qinling Mountains, and the Shuangwang gold deposit is a representative large-sized deposit of auriferous albite breccias type in this area. Based on Gregorian’s zoning index method, the authors studied the vertical zoning characteristics of primary halos at the depth of drill holes ZK18-5, ZK30-1, and ZK40-5 in orebodies KT9 and KT8. By discussing the vertical variation of the zoning rate of primary halos, the graphical method of 3-end-mumber diagram, and the vertical change rules of the geochemical parameter, the authors hold that the orebody indicated by ZK18-5 thins out gradually at the depth, with a higher degree of mineralization at the elevation of 950 m; bead-shaped orebodies may occur at the depth of ZK30-1, with a higher degree of mineralization at the elevation of 980 m; the ore body indicated by ZK40-5 with a higher degree of mineralization at the elevation of 850 m still extends to the depth without pinching out.

       

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