山西盂县王子台——南小坪铝土矿矿床地质特征及其成因分析  

Geological Characteristics and Genesis Analysis of the Wangzitai Nanxiaoping Bauxite Deposit in Yu County,Shanxi Province

作　　者：郭政斌 王浩乾 刘安 王明明 GUO Zheng-bin;WANG Hao-qian;LIU An;WANG Ming-ming(No.3 Bureau of China Metallurgical Geology Bureau,Taiyuan 030000,China)

机构地区：[1]中国冶金地质总局三局,山西太原030000

出　　处：《中国非金属矿工业导刊》2020年第3期29-31,共3页China Non-Metallic Minerals industry

摘　　要：山西省盂县王子台-南小坪矿区铝土矿属泻湖-浅海相沉积型铝土矿床。矿体赋存于石炭系中统本溪组下段地层中。根据矿体分布范围及特征对其划分为3个矿体,其矿石工业类型为一水硬铝石型低硫含铁型铝土矿,矿石品级为Ⅳ级。石炭系本溪组地层是寻找铝土矿的重要找矿标志。The Wangzitai Nanxiaoping bauxite deposit in Yu County,Shanxi Province is a lagoon shallow sea sedimentary bauxite deposit.The ore body occurs in the lower part of Benxi Formation of Middle Carboniferous.According to the distribution scope and characteristics of the ore body,it is divided into three ore bodies.The ore industry type is diaspore type low sulfur iron bearing bauxite,and the ore grade is IV.Benxi Formation of Carboniferous is an important prospecting indicator for bauxite.

关 键 词：铝土矿 地质特征 成因分析 盂县 

分 类 号：P618.45[天文地球—矿床学]