姜能. 小秦岭金矿床的成矿物质来源[J]. 地质与资源, 1995, 4(4): 269-274.
    引用本文: 姜能. 小秦岭金矿床的成矿物质来源[J]. 地质与资源, 1995, 4(4): 269-274.
    Jiang Neng. THE SOURCE OF ORE-FORMING MATERIALS IN XIAOQINLING GOLD DEPOSITS[J]. Geology and Resources, 1995, 4(4): 269-274.
    Citation: Jiang Neng. THE SOURCE OF ORE-FORMING MATERIALS IN XIAOQINLING GOLD DEPOSITS[J]. Geology and Resources, 1995, 4(4): 269-274.

    小秦岭金矿床的成矿物质来源

    THE SOURCE OF ORE-FORMING MATERIALS IN XIAOQINLING GOLD DEPOSITS

    • 摘要: 研究表明,太华群是小秦岭地区金矿床的矿源层。通过对比混合岩化、花岗岩化、围岩蚀变和成矿作用过程中的微量元素的分布情况,发现Au和Pb、Cu、Ag、Zn等在这一系列过程中始终表现出变化的一致性,说明Au等成矿物质来源于太华群变质岩,同位素证据也表明Au等成矿物质来源于太华群。

       

      Abstract: Based on the geological development history of Xiaoginling district, Taihua group is considered the possible source bed of ore-forming materials of Xiaoqinling gold deposits, The concentration changes of trace elements of rocks and/or ore throughout migmatitization, granitization, alteration and mineralization show that the changes of Au concentration is inaccordane with that of other ore-forming materials such as Pb, Cu, Ag, Zn, etc. all the time。It suggests that the ore-forming materials come from Taihua group.Furthermore, isotopic data also show the ore-forming materials come from Taihua group.

       

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