摘要
广西平南县上龙稀土矿区位于南岭成矿带的西南部,是中国离子吸附型稀土矿的矿化集中区。上龙风化壳离子吸附型稀土矿床产于花岗岩体风化壳中,成矿与华力西期六陈岩体、华力西-印支期大容山岩体关系密切。文章在前人研究的基础上,通过对平南县上龙稀土矿床的地质背景、矿体地质、成矿规律、成矿模式进行深入总结研究,为下一步勘查提供依据,对于区内其他地段开展找矿具有重要的指导意义。
The Shanglong rare earth mining area in Pingnan County,Guangxi is located in the southwest of the the Nanling Mountain metallogenic belt,and is a concentration area of ion adsorption type rare earth deposits in China.The Shanglong weathering crust ion adsorption type rare earth ore occurs in the weathering crust of the Hualixi Liuchen rock mass and the Hualixi Indosinian Darongshan rock mass,and its mineralization is closely related to the Liuchen rock mass and Darongshan rock mass.On the basis of previous research,this paper conducts in-depth summary and research on the geological background,ore body geology,ore-forming laws,and ore-forming models of the Shanglong rare earth deposit in Pingnan County,providing a basis for the next exploration and having important guiding significance for mineral exploration in other areas within the area.
作者
韦东广
WEI Dong-guang(Guangxi Zhuang Autonomous Region 307 Nuclear Geological Brigade,Guigang 537100,China)
出处
《世界有色金属》
2024年第2期81-83,共3页
World Nonferrous Metals
关键词
广西平南县
上龙
离子吸附型
成矿模式
Pingnan County,Guangxi
Shanglong
Ion adsorption type
Metallogenic model
作者简介
韦东广,男,生于1988年,壮族,广西贵港人,本科,工程师,研究方向:地质矿产勘查。
