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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,2009,23(3):258-260,267.
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  太古宙绿岩带  前寒武系变质岩  破碎蚀变岩型  找矿意义

Geological feature and prospecting significance of connemara gold deposit in Zimbabwe
LI Ru-man,LIU Feng,LIU Feng-juan.Geological feature and prospecting significance of connemara gold deposit in Zimbabwe[J].Mineral Resources and Geology,2009,23(3):258-260,267.
Authors:LI Ru-man  LIU Feng  LIU Feng-juan
Institution:(Tianjin North China Geological Exploration Bureau, Tianjing 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.It is the type of gold deposit hosted in altered fracture belts.The wall rock alterations are well developed.Silicification,pyritization and sericitization are closely related to the mineralization.There is a good prospecting potential in the mine.
Keywords:gold deposit  Archean greenstone belt  Precambrian metamorphic rocks  fractured and altered rock type  prospecting significance
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