摘要
天堂山矿区铷锡多金属矿地处北北东向武夷山多金属成矿带南段与南岭纬向多金属成矿带东端的交汇部位,近几年的勘探地质工作加强了矿区成矿地质特征研究,特别是对深部岩体、构造空间方面及蚀变岩体的研究,同时结合物、化探成果资料,深部钻探等多元信息分析,获得了新的认识,矿区铷锡多金属矿找矿成果显著,尤其是铷的找矿工作取得了重大突破,目前已探明的Rb2O资源量属超大型矿床规模。
The Rb Sn polymetallic ore deposit in the Tiantangshan mining area is located at the intersection of the southern section of the NNE trending Wuyishan polymetallic metallogenic belt and the eastern end of the Nanling latitudinal polymetallic metallogenic belt.The exploration and geological work in recent years has strengthened the research on the metallogenic geological characteristics of the mining area,especially on the deep rock mass,structural space and altered rock mass.At the same time,in combination with the analysis of geophysical and geochemical results,deep drilling and other multiple information,new understanding has been obtained,Remarkable achievements have been made in the exploration of rubidium tin polymetallic ore deposits in the mining area,especially the major breakthrough has been made in the exploration of rubidium.At present,the proven Rb2O resources are of super large scale.
作者
郭克林
陈贵玖
吴俊刚
GUO Ke-lin;CHEN Gui-jiu;WU Jun-gang(Hunan Provincial Ecological Geological Survey and Monitoring Institute,Changsha 410000,China;Hunan Provincial Mineral Resources Survey Institute,Changsha 410131,China)
出处
《世界有色金属》
2023年第7期82-84,共3页
World Nonferrous Metals
关键词
铷锡多金属矿
地质特征
新认识
找矿突破
Rb Sn polymetallic ore
geological characteristics
new understanding
ore prospecting breakthrough