摘要
牦牛坪稀土矿床具有规模大、埋藏浅、有用矿物晶体粗大、易采易选、有益伴生组份多、多阶段成矿、成矿地质条件及成因类型独特等特点,是以岩浆—热液充填为主形成的碱性花岗岩、伟晶岩—碳酸岩型稀土矿床.
The Maoniuping Rare earth element deposit is characterized by its peculier geological conditions and genetic types. The deposit is large in size and shallow in hurried depth, with useful orc minerls of coarse crystallized grains, easily to be dressed and mined, and many different useful associated components. It is of multiple genesis and belongs to the type formed in alkali-granite, pegmatite carbonate rock produced by mainly magmatic-hydrothermal fissure filling.
出处
《地质与勘探》
CAS
CSCD
北大核心
1991年第5期18-23,共6页
Geology and Exploration
