论文部分内容阅读
用惰性元素组分TiO2的质量系数作为参考点，定量估算了热液蚀变过程中主量元素和微量元素的迁移特性，探讨了元素迁移的地球化学性状及其与蚀变类型的关系，指出As、Sb、Cu、Ph、Zn可以作为成矿的指示元素，硅化、黄铁矿化、绢英岩化蚀变与成矿关系密切，热液蚀变对成矿作用有明显的影响。
Using the mass coefficient of TiO2, an inert element, as a reference point, the migration characteristics of major and trace elements during hydrothermal alteration were quantitatively estimated. The geochemical characteristics of migration and their relationship with alteration types were also discussed. As, Sb, Cu, Ph and Zn can be used as indicator elements for metallogenesis. Silification, pyrite and sericite alteration are closely related to metallogenesis, and hydrothermal alteration has obvious influence on mineralization.