摘要
在总结前人研究基础上,对书楼丘铀矿床赋矿围岩、含矿构造、矿体特征、成矿温度、蚀变矿物组合等进行分析研究,结果表明该矿床为中低温热液成因矿床,成矿时代为燕山晚期。通过对矿区内矿床地质以及地球物理研究表明,书楼丘矿床深部具有良好的找矿潜力,是下一步找矿的重点方向。
Based on previous research,the analysis and study of the ore-bearing surrounding rock,ore-bearing structure,ore body characteristics,ore-forming temperature,altered mineral combinations,etc.are carried out in Shulouqiu uranium deposit,and the results show that the deposit is a mid-low temperature hydrothermal deposit and the ore-forming age is in the late Yanshanian.The geological and geophysical researches on the deposit show that the potential for prospecting the Shulouqiu deposit is in the deep of the ore and which is the key direction for further exploration.
作者
张善果
ZHANG Shan-guo(Shaoguan Jinyuan Uranium Co.,Ltd.,CNNC,Shaoguan 512328,China)
出处
《铀矿冶》
CAS
2019年第2期157-164,共8页
Uranium Mining and Metallurgy
关键词
花岗岩型铀矿
地质特征
矿床成因
找矿潜力
granite-type uranium deposit
geological characteristics
ore genesis
prospecting potential