青嶂山岩体黄沙铀矿区铀成矿地质条件及找矿潜力浅析  

Analysis of Geological Condition and Prospecting Potential of Uranium Metallogenesis in Huangsha Uranium District,Qinzhangshan Rock Mass

作　　者：牟平[1] 

机构地区：[1]东华理工大学放射性地质与勘探技术国防重点学科实验室,江西南昌330013

出　　处：《绿色科技》2016年第14期242-244,共3页Journal of Green Science and Technology

摘　　要：指出了青嶂山岩体是一个由多期多阶段岩浆侵入形成的复式花岗岩体,可视为诸广山岩体的一部分,被南雄断陷带割裂。黄沙铀矿区产于青嶂山复式岩体中南部,区内构造发育,热液活动频繁,热液蚀变作用强烈,具有得天独厚的铀成矿地质条件,有较大的找矿潜力。Qingzhangshan rock mass is acompound granite masswhich is formed by multi--stages magma intrusion, which can be considered as part of the Zhuguangshan rock mass.It is dissevered by Nanxiong fault--subsiding belt. Huangsha uranium mine area is located in the south central partof Qingzhangshan complex mass whose the tectonic activity development and hydrothermal activity are frequent and hydrothermalalteration effect is strong. It has a unique uranium mineralization geological conditions and great prospecting potential.

关 键 词：青嶂山岩体 黄沙铀矿区 铀成矿 找矿潜力 

分 类 号：P619.14[天文地球—矿床学]