| 云南腾冲茨竹地铁多金属矿矿床成因 |
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| 引用本文： | 陈海军,李建洪,田燕红,白平.云南腾冲茨竹地铁多金属矿矿床成因[J].云南地质,2010,29(2):156-159. |
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| 作者姓名： | 陈海军 李建洪 田燕红 白平 |
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| 作者单位： | 1. 云南省地质工程勘察总公司,昆明,650051
2. 云南省国土资源厅,昆明,650224 |
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| 摘 要： | 矿体赋存于地盘关燕山早期花岗岩与上石炭统空树河组接触带中。磁铁矿为主,伴生黑钨矿、锡石等。矽卡岩化与成矿关系密切,黑云母二长花岗岩应是成矿母岩。
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| 关 键 词： | 铁多金属矿 高中温钙矽卡岩 破碎带赋矿 与花岗岩有关 云南腾冲茨竹地 |
THE GENESIS OF CIZHUDI FE MULTIMETALLIC DEPOSIT IN TENGCHONG,YUNNAN |
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| CHEN Hai-jun,LI Jian-hong,TIAN Yan-hong,BAI Ping.THE GENESIS OF CIZHUDI FE MULTIMETALLIC DEPOSIT IN TENGCHONG,YUNNAN[J].Yunnan Geology,2010,29(2):156-159. |
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| Authors: | CHEN Hai-jun LI Jian-hong TIAN Yan-hong BAI Ping |
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| Institution: | 1.Yunnan Geoexploration Company General,Kunming 650051)(2.Yunnan Department of Land Resources,Kunming 650224) |
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| Abstract: | The ore body is in the contact between Early Yanshanian Dipanguan granite and Upper Carboniferous Kongshuhe Formation.The main ore mineral is magnetite,with associated wolframite,cassiterite,etc.The metallogenesis is close related with skarnization.The biotite adamellite must be the mother rock of metallogenesis. |
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| Keywords: | Fe Multimetallic Deposit High-Middle T Calc-Skarn Ore-Bearing of Fracture Zone Related to Granite Cizhudi Tengchong Yunnan |
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