河北邢台县卫鲁蓝晶石矿地质特征研究  

GEOLOGICAL CHARACTERISTICS OF THE WEILU KYANITE IN XINGTAI, HEBEI PROVINCE

作　　者：温小亚 郎志杰 楚山巍 

机构地区：[1]中钢石家庄工程设计研究院有限公司,河北石家庄050021

出　　处：《化工矿产地质》2016年第3期151-155,共5页Geology of Chemical Minerals

摘　　要：卫鲁蓝晶石矿是一个大型的蓝晶石矿床,区内矿床呈层状、似层状、透镜状,矿体均赋存在太古界放甲铺组中,矿床成因类型为火山沉积变质矿床。石榴蓝晶黑云斜长片麻岩型是本区的主要矿石类型,蓝晶石平均品位为13.17%。矿床开采技术条件属简单类型。通过本次系统的地质特征研究,能够为该矿山合理进行采矿设计、安全开采等提供较为详细的基础资料,为矿区外围及深部地质勘查提供依据。In this paper, mine geology, ore deposit geological characteristics, ore quality and mining technical conditions of the WeiLu Kyanite is studied. This mine is a large volcanic sedimentary metamorphic ore deposits, in which ore deposits are layered, stratified, lenticular and orebody occurrence in Fangjiapu formation of the Archeozoic. Aquamarine biotite plagioclase gneiss is the main ore type and the average grade of Kyanite is 13.17%. Deposit mining conditions is relatively simple. The system study on the geological characteristics can provide detailed data for mining design and safe mining, at the same time, provide the basis for peripheral and deep geological exploration.

关 键 词：卫鲁 蓝晶石 地质特征 

分 类 号：P619.281[天文地球—矿床学]