摘要
The Banian sediment-hosted antimony deposit is a medium-scale deposit located in the Dushan County,South Guizhou,China.Calcite as the dominant gangue mineral can be divided into two types: white and pink,the later is more intimate with mineralization.It is interesting that the REE characteristics are
作者
WANG Jia-sheng1,2,WEN Han-jie2,FAN Hai-feng2,ZHU Jing-jing1,2,ZHANG Jin-rang1,2(1.State Key Laboratory of Ore Deposit Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences,Guiyang 550002,China
2.Graduate School of Chinese Academy of Science,Beijing,100039,China)
出处
《矿物学报》
CAS
CSCD
北大核心
2011年第S1期642-642,共1页
Acta Mineralogica Sinica
