| 云南勐腊新山铁多金属矿矿化富集规律 |
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| 引用本文： | 赵含军,范建辉,廖锦川.云南勐腊新山铁多金属矿矿化富集规律[J].云南地质,2011,30(2):157-159. |
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| 作者姓名： | 赵含军 范建辉 廖锦川 |
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| 作者单位： | 云南黄金矿业集团勘查院,云南昆明,650215 |
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| 摘 要： | 新山铁多金属矿矿床规模大、品位高、共（伴）生有铜铅锌银等多种有用组份。经历了火山（海相）喷发、生物化学沉积、成岩作用、地下热水循环改造等多期成矿阶段,属火山喷发沉积—改造（层控碳酸盐）型矿床。
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| 关 键 词： | 铁铜铅锌银矿 层状脉状残坡积 上三叠统大路边组 浅海碳酸盐沉积 云南勐腊新山 |
THE METALLOGENETIC CONCENTRATION RULE OF XINGSHAN FE MULTIMETALLIC DEPOSIT IN MENGLA, YUNNAN |
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| ZHAO Han-jun,FAN Jian-hui,LIAO Jin-chuan.THE METALLOGENETIC CONCENTRATION RULE OF XINGSHAN FE MULTIMETALLIC DEPOSIT IN MENGLA, YUNNAN[J].Yunnan Geology,2011,30(2):157-159. |
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| Authors: | ZHAO Han-jun FAN Jian-hui LIAO Jin-chuan |
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| Institution: | ZHAO Han-jun,FAN Jian-hui,LIAO Jin-chuan(Yunnan Exploration Institute of Au Mining Group,Kunming 650215) |
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| Abstract: | It is a large scale,high grade multimetallic deposit with many paragenetic elements,such as Cu,Pb,Zn,Ag,etc.It has experienced the volcanic eruption（marine facies）,biochemical sedimentation,diagenesis and cyclic reformation of underground thermal fluid,which belongs to the ore deposit of volcanic eruption sedimentation—reformation（stratabound carbonate）type. |
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| Keywords: | Fe-Cu-Pb-Zn-Ag Deposit Bedded Veined Eluvium-Slope Wash Upper Triassic Dalubian Formation Neritic Carbonate Sediment Xingshan Mengla Yunnan |
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