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黑龙江老柞山金矿地球化学特征及成因模式
THE GEOCHEMISTRY AND FORMATION MODEL FOR THE LAOZUOSHAN GOLD DEPOSIT IN HEILONGJIANG
【摘要】 老柞山金矿是黑龙江重要的黄金产地之一。本文对该金矿床的成矿地质背景和硫同位素、铅同位素、碳和氧同位素的组成特征进行了分析研究。结果显示成矿流体类型为来源于壳幔同熔的混合含矿岩浆热液,成矿物质主要来自幔源或少量地壳物质。矿石和岩浆岩具有非常相似的铅同位素组成,暗示了二者的亲缘关系。在综合已有地质资料的基础上,对矿床的成因模式进行了总结,强调该矿床的形成是多次构造岩浆逐步富集而成。
【Abstract】 This paper deals with the Laozuoshan gold deposit,one of the important gold mines in Heilongjiang province,its geological background and isotopic elements such as sulphur,lead,carbon,and oxygen.The studies indicate that the ore-bearing fluid is magma with minor crust and major mantle substances.The ore and the magma share similar lead isotopic features which suggests a close relations between them.The authors consider that the Laozuoshan gold deposit is resulting from multiple tectono-magmtic activities.
【关键词】 同位素组成;
成因模式;
老柞山金矿;
【Key words】 isotopic elements; metallogenic model; Laozuoshan gold deposit;
【Key words】 isotopic elements; metallogenic model; Laozuoshan gold deposit;
- 【文献出处】 资源环境与工程 ,Resources Environment & Engineering , 编辑部邮箱 ,2006年02期
- 【分类号】P618.51
- 【被引频次】6
- 【下载频次】254