广西钦州地区稀土矿床地质特征及成因探讨  

On the Geological Characteristics and Genesis of Rare Earth Deposits in Qinzhou Region of Guangxi

作　　者：韦意谊[1] 

机构地区：[1]广西壮族自治区第三地质队,广西钦州535000

出　　处：《能源与节能》2014年第5期81-83,共3页Energy and Energy Conservation

摘　　要：从矿床的矿物学和矿床地质特征出发,认为广西钦州地区稀土矿床是有较高稀土丰度的母岩,在有利条件下,经过风化作用,最终在风化壳中形成离子吸附型稀土矿床。结合在该地区进行的相关地质工作,对稀土矿床地质特征及成因进行相关探讨,并认为在相似的地质条件下,有找到类似矿床的前景。According to the mineralogical and geological characteristics of the deposit, it is considered that the rare earth depositsin Qinzhou region of Guangxi is ion-absorbing type rare earth deposits formed with parent rock with a high abundance of rareearth after weathering under favorable conditions in crust of weathering. Discusses the geological characteristics and causes of rareearth deposits combining with the related geological work carried out in the area, and considers that it is of prospects of findingsimilar deposits in similar geological conditions.

关 键 词：钦州地区 稀土 地质特征 矿床成因 

分 类 号：P618.7[天文地球—矿床学]