摘要
伏牛山矿床位于扬子准地台下扬子台褶束带南京坳陷的北东地段的淮阳山字型东翼反射弧上.伏牛山铜铁铅锌矿床其形成于晚古生代,成因上与矿区内的围岩、岩浆岩及断裂构造关系密切.文章在对伏牛山矿区及外围野外地质调研工作的基础上,通过对区域成矿地质背景矿床地质特征等详实研究、收集样品进行稀土元素地球化学分析、构建矿区三维空间模型等方法,重点深入研究分析了伏牛山岩浆岩和断裂构造对矿体产出空间的控制作用、矿体空间形态和展布特征以及伏牛山矿床控矿因素分析.
The Funiushan deposit is located in the Ningzhen area, the eastern of the middle and lower Yangtze iron and copper metallogenic belt. The Funiushan copper-iron deposit was formed in the Late Paleozoic, and its genesis is closely re- lated to the host rock, magmatic rock and fault structure. Based on the filed work and geological research of the Funiushan mining area, the geological characteristics of the mineralization of the regional metallogenic geological prospect are studied , the rare earth element geochemical characteristics of the collected samples are analyzed, and the three-dimensional spatial model of the mining area is constructed. The control effect of the Funiushan magmatic rock and the fault structure on the ore body, the spatial morphology and distribution of the ore body and the ore-controlling factors of the Funiushan deposit are an- alyzed in detail.
出处
《南方金属》
CAS
2017年第5期24-28,共5页
Southern Metals
基金
国家自然科学基金资助项目(41240017和41372338)
