摘要
邓广圩-太平铝土矿床赋存于第四系残坡积红土层中,有埋藏浅、规模大、分布广的特点.矿床受矿源层、地层岩性、构造、地貌、气候等因素控制.结合区域矿床对比,初步认为该矿床成因类型为堆积型三水铝土矿床.在矿床地质背景基础上,着重研究分析了矿床的控矿因素,认为该区具有较好的铝土矿成矿地质条件和找矿前景,是寻找大中型铝土矿的有利地区.
The Dengguangxu-Taiping bauxite deposit,occurring in the Quaternary residual talus laterite,is characterized by shallow buries,large scale and broad distribution.The ore deposit is controlled by the resource bed,lithology,structure,landform and climate.With comparison to the regional deposits,it is believed that the genetic type of this deposit is of accumulated gibbsite deposit.Analysis of the ore-controlling factors on the basis of geological background proves that,with advantageous geological conditions and good exploration prospect,this area is favorable for medium and large sized bauxite deposits.
出处
《地质与资源》
CAS
2014年第2期170-173,共4页
Geology and Resources
关键词
铝土矿
控矿因素
找矿前景
邓广圩-太平
广西
bauxite
ore-controlling factor
prospect
Dengguangxu-Taiping
Guangxi
