摘要
自然铝赋存于莲花山斑岩型钨矿区的石英闪长玢岩和蚀变石英砂岩中,呈不规则粒状,一般粒径0.2～0.04mm,淡黄-白色,浸染于脉石矿物中.Al含量低于前人发现的自然铝.
Native aluminum was discovered in quartz dioritic porphyrite and altered quartz sandstone in theLianhuashan tungsten mining district. It has an irregular grain shape, usually 0.2-0.04mm in size andwhite in colour, and occurs as impregnation ore in gangue minerals. The alumiunm content of the Lianhuashan W-deposit area is lower than those of previous discoveries.
出处
《地质与勘探》
CAS
CSCD
北大核心
1990年第9期32-34,共3页
Geology and Exploration
