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云南潞西大矿山铅锌矿
引用本文:武龙祥,李志坚,罗显辉,丁海宏,刘世维.云南潞西大矿山铅锌矿[J].云南地质,2008,27(2):197-202.
作者姓名:武龙祥  李志坚  罗显辉  丁海宏  刘世维
作者单位:云南省有色地质楚雄勘查院,云南,楚雄,675000
摘    要:矿体产于花岗岩以上断层附近大理岩中,大理岩与花岗岩接触部位是主要的矿化部位,在大矿山、小石林、灰窑等地见有强褐铁矿化、弱铅锌矿化的厚大矿化层。通过勘查工作,认为矿区具有寻找中-大型规模矿山的前景。

关 键 词:矿床地质特征  矿床成因  大矿山  潞西  云南

THE DAKUANGSHAN PB ZN DEPOSIT OF LUXI, YUNNAN
WU Long-xiang,LI Zhi-jian,LUO Xian-hui,Ding Hai-hong,LIU Shi-wei.THE DAKUANGSHAN PB ZN DEPOSIT OF LUXI, YUNNAN[J].Yunnan Geology,2008,27(2):197-202.
Authors:WU Long-xiang  LI Zhi-jian  LUO Xian-hui  Ding Hai-hong  LIU Shi-wei
Institution:( Chuxiong Institute of Nonferrous Geological Exploration of Yunnan Province, Chuxiong 675000)
Abstract:The ore body exists in the marble, which is near the fault and over the granite. The contact between marble and granite is the main metallogenetic part. There is a thick metallogenetic bed of intense ferritization and weak Pb - Zn metallogenesis at Dakuangshan, Xiaoshilin and Huiyao, etc. According to the exploration, we believe that this orefield has the prospects of finding out a middle- large scale ore deposit.
Keywords:Geological Characteristics of Ore Deposit  Genesis of Ore Deposit  Dakuangshan  Luxi  Yunnan
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