| 云南泸水双米地铅矿成因探讨 |
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| 引用本文： | 刘仕军,和松文.云南泸水双米地铅矿成因探讨[J].云南地质,2013(4):417-420. |
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| 作者姓名： | 刘仕军 和松文 |
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| 作者单位： | 云南地矿国际矿业公司,云南昆明650051 |
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| 摘 要： | 脉状矿体赋存于高黎贡山群下亚群第三层（Ptgl31）,品位取决于大理岩、片麻岩破碎程度,典型的中低温热液裂隙充填型铅矿.
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| 关 键 词： | 充填脉状铅矿 次级断裂破碎带 大理岩一片麻岩 高黎贡山群 云南泸水双米地 |
A PROBE INTO THE GENESIS OF SHUANGMIDI PB DEPOSIT IN LUSHUI,YUNNAN |
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| LIU Shi-jun,HE Song-wen.A PROBE INTO THE GENESIS OF SHUANGMIDI PB DEPOSIT IN LUSHUI,YUNNAN[J].Yunnan Geology,2013(4):417-420. |
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| Authors: | LIU Shi-jun HE Song-wen |
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| Institution: | ( Yunnan Company of International Geology ＆ Mining Industry, Kunming 650051 ) |
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| Abstract: | The veined ore body is in Gaoligongshan Group Lower Subgroup the 3rd bed （ Ptgf13 ）. The grade is determined by the fracture degree of the marble and the gneiss. It is a typical middle - low T hydrothermal Pb de- posit of fissure filling type. |
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| Keywords: | Filling Veined Pb Deposit Secondary Fault Fracture Zone Marble - Gneiss GaoligongshanGroup Shuangmidi Lushui Yunnan |
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