论文部分内容阅读
论述了灵山沟金矿床的地球化学特征、不同成矿阶段的元素组合及原生晕的垂直分带规律，建立了矿床的叠加成矿成晕模式，用模式进行了预测。
The geochemical characteristics of the Lingshangou gold deposit, the vertical assemblages of the primary halo and elemental assemblages in different mineralization stages are discussed. The superimposed mineralization and halo formation of the ore deposit are established and predicted by the model.