| 云南勐海关双铁矿矿床成因 |
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| 引用本文： | 王爱萍,高李阳,张吉寿.云南勐海关双铁矿矿床成因[J].云南地质,2011,30(2):160-163. |
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| 作者姓名： | 王爱萍 高李阳 张吉寿 |
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| 作者单位： | 云南黄金矿业集团股份有限公司,云南昆明,650224 |
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| 摘 要： | 关双铁矿位于大南婆—惠民—西定金多金属矿富集区。矿床成因与澜沧惠民铁矿类似,属海相火山沉积变质型。
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| 关 键 词： | 沉积变质铁矿 海相火山堆积 富铁辉绿岩 云南勐海关双 |
THE GENESIS OF GUANSHUANG FE DEPOSIT IN MENGHAI,YUNNAN |
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| WANG Ai-ping,GAO Li-yang,ZHANG Ji-shou.THE GENESIS OF GUANSHUANG FE DEPOSIT IN MENGHAI,YUNNAN[J].Yunnan Geology,2011,30(2):160-163. |
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| Authors: | WANG Ai-ping GAO Li-yang ZHANG Ji-shou |
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| Institution: | WANG Ai-ping,GAO Li-yang,ZHANG Ji-shou(Yunnan Company(Ltd)of Au Mining Group,Kunming 650224) |
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| Abstract: | The Guanshuang Fe deposit is in the Dananpo-Huimin-Xiding Au multimetallic concentration area.The genesis of ore deposit is similar to that of Huimin Fe deposit in Lancang,which belongs to the Fe deposit of marine volcanic sedimentation metamorphic type. |
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| Keywords: | Sedimentary Metamorphic Fe Deposit Marine Volcanic Accumulation Metallogenetic Model Factor of Ore Control Guanshuang Menghai Yunnan |
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