摘要
福建宁化上畲矿区稀土矿位于福建省离子吸附型稀土矿重要成矿带:光泽—武平Ⅲ级成矿带之宁化—清流Ⅳ级成矿远景区内。其含矿岩体分布广,成矿条件优越。在矿区勘查的基础上,从成矿特征,矿体富集规律等方面对离子稀土矿床特征进行了初步总结,并分析了矿床成因和找矿标志。
The rare earth deposits in Shangshe mining area of Ninghua, Fujian Province are located in the Ninghua Qingliu IV metallogenic prospect area of Guangze Wuping III metallogenic belt, an important metallogenic belt of ion adsorption type rare earth deposits in Fujian Province. The ore bearing rocks are widely distributed and the metallogenic conditions are superior. Based on the exploration of the mining area, the characteristics of the ion rare earth deposits are preliminarily summarized from the aspects of metallogenic characteristics, ore body enrichment laws, etc., and the genesis of the deposits and prospecting indicators are analyzed.
作者
洪鑫源
HONG Xin-yuan(Fujian Second Geological Exploration Brigade,Yong'an 366000,China)
出处
《世界有色金属》
2022年第20期107-109,共3页
World Nonferrous Metals
关键词
成矿特征
稀土矿
离子吸附型
宁化上畲
metallogenic characteristics
Rare earth ore
Ion adsorption type
Ninghua Shangshe
