首页 | 本学科首页   官方微博 | 高级检索  
     检索      

浅论津巴布韦康尼玛拉(Connemara)金矿床地质特征及其找矿意义
引用本文:李如满,刘峰,柳凤娟.浅论津巴布韦康尼玛拉(Connemara)金矿床地质特征及其找矿意义[J].矿产与地质,2010,24(3):210-212,240.
作者姓名:李如满  刘峰  柳凤娟
作者单位:天津华北地质勘查局,天津,300181
摘    要:康尼玛拉金矿床的形成与太古宙绿岩带、前寒武系变质岩关系密切,矿体、矿化蚀变体主要受NNW向断裂构造控制,属破碎蚀变岩型金矿,围岩蚀变发育,硅化、黄铁矿化、绢云母化与矿化关系密切,该矿区具有良好的找矿前景。

关 键 词:金矿床  地质特征  破碎蚀变岩型  找矿意义

Discussion on geological characteristics and prospecting significances of Connemara gold deposit in Zimbabwe
LI Ru-man,LIU Feng,LIU Feng-juan.Discussion on geological characteristics and prospecting significances of Connemara gold deposit in Zimbabwe[J].Mineral Resources and Geology,2010,24(3):210-212,240.
Authors:LI Ru-man  LIU Feng  LIU Feng-juan
Institution:(Tianjin North China Geological Exploration Bureau,Tianjin 300181)
Abstract:Connemara gold deposit is associated with Archean greenstone belt and Precambrian metamorphic rocks.The orebody and altered belts are controlled by NNW trending faults,which is the type of gold deposit hosted in altered fracture belts.The wall rock alterations are well developed,such as silicification,pyritization,sericitization etc,which is closely related to the mineralization.It has a good prospects in this ore field.
Keywords:gold deposit  geological characteristic  fracture zone altered rock type  prospecting significances
本文献已被 维普 万方数据 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号