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云南德钦良通铅锌矿控矿地质条件
引用本文:孟富军,李志刚,白媛媛.云南德钦良通铅锌矿控矿地质条件[J].云南地质,2011,30(2):151-153.
作者姓名:孟富军  李志刚  白媛媛
作者单位:云南省地质矿产勘查院大理地质矿产所,云南大理,671000
摘    要:良通铅锌矿产于印支期石英闪长岩(δο15)内部裂隙、破碎带内,控矿因素为岩浆岩、岩浆岩侵位的地层、构造等,中低温热液型铅锌多金属矿床,矿区及外围具有较大的找矿前景。

关 键 词:中低温热液型  铅锌多金属矿  岩浆岩内破裂带  印支期闪长岩  云南德钦良通

THE ORE CONTROL GEOLOGICAL CONDITION OF LIANGTONG PB- ZN DEPOSIT IN DEQIN, YUNNAN
MENG Fu-jun,LI Zhi-gang,BAI Yuan-yuan.THE ORE CONTROL GEOLOGICAL CONDITION OF LIANGTONG PB- ZN DEPOSIT IN DEQIN, YUNNAN[J].Yunnan Geology,2011,30(2):151-153.
Authors:MENG Fu-jun  LI Zhi-gang  BAI Yuan-yuan
Institution:MENG Fu-jun,LI Zhi-gang,BAI Yuan-yuan(Dali Institute of Geology & Mineral Resources,Yunnan Exploration Institute of Geology & Mineral Resources,Dali 671000)
Abstract:The Liangtong Pb-Zn deposit is in the inner fissure fracture zone of Indosinian quartz diorite(δo15).The ore control factors are the magmatic rock,strata and structure of magmatic rock emplacement,which is a Pb-Zn multimetallic deposit of middle-low T hydrothermal type.There is very good potentiality of ore prospecting in the orefield and the area around it.
Keywords:Middle-Low T Hydrothermal Type  Pb-Zn Multimetallic Deposit  Inner Fracture Zone of Magmatic Rock  Indosinian Diorite  Liangtong  Deqin  Yunnan  
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