摘要
永平过碱性杂岩体因有利的成矿条件,形成了风化壳型磷灰石稀土(砂)矿床。稀土元素的主要赋存形式有离子吸附型和类质同像两种类型,重砂矿物主要为磷灰石、磁铁矿等,还见少量独居石。磷灰石作为主要的赋矿矿物,稀土氧化物含量较高。
The Yongping super-alkaline complex has formed weathering crust type apatite rare earth(sand)deposit because of favorable ore-forming conditions.The main occurrence forms of rare earth elements are ion adsorption type and ISOMORPHISM type.The heavy placer minerals are mainly apatite,magnetite and a few monazite.As the main ore-bearing mineral,apatite has high content of rare earth oxides.
作者
汪永华
王艳
WANG Yong-hua;WANG Yan(Geological Institute,Yunnan Bureau of Nonferrous Geology,Kunming 650216,China;Yunnan Bureau of nonferrous Geology,Kunming 650051,China)
出处
《世界有色金属》
2020年第22期206-207,共2页
World Nonferrous Metals