摘要
本文通过对矿床地质特征的分析,探讨区域地质背景、构造、岩浆岩、围岩蚀变与成矿之间的关系。矿区内矿体严格受断裂构造控制;成矿与硅化、黄铁矿化、方解石化关系密切,和硅化强烈的混合花岗岩、武功山二长花岗岩有关。
This article analyzes the geological characteristics of the deposit,exploring the relationship between regional geological background,tectonic,magmatic rock,wall rock alteration and mineralization.The ore body in the mining area is strictly controlled by fault structure,Mineralization is closely related to silicification,pyrite mineralization and resolving.It is related to the strong silicified mixed granite and the second long granite of Wugong Mountain.
作者
游伟华
方磊
刘伯乐
YOU Wei-hua;FANG Lei;LIU Bo-le(No.266 Geological Party,Jiangxi Bureau of Nuclear Industry Geology,Nanchang 330038,China)
出处
《世界有色金属》
2019年第19期136-136,138,共2页
World Nonferrous Metals
关键词
年坑
银铅矿床
地质特征
控矿因素
Ningkeng Silver
lead deposit
Geological Features
Ore controlling factor
