| 云南兰坪罗善铅锌矿控矿因素及成因 |
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| 引用本文： | 徐兴业,黄发梅,张桂银,苏泰民,黄联飞.云南兰坪罗善铅锌矿控矿因素及成因[J].云南地质,2013(4):421-423,416. |
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| 作者姓名： | 徐兴业 黄发梅 张桂银 苏泰民 黄联飞 |
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| 作者单位： | [1]云南省地质矿产勘查院大理地质矿产所,云南大理671000 [2]云南省地质矿产勘查院昆明快速勘查评价所,云南昆明650051 [3]云南地矿总公司地质矿产勘查二院,云南昆明650051 |
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| 摘 要： | 铅锌矿赋存于上三叠统三合洞组下段（T3s1）灰岩容矿岩层中及近南北向、北北东向、北西向断裂破碎带内,少数赋存在近东西向节理裂隙中,成因具多成矿阶段、多成矿物质来源特征,层位＋构造控制的中低温热液型铅锌多金属矿床.
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| 关 键 词： | 中低温热液矿床 矿床成因 地层构造控矿 云南兰坪罗善 |
THE ORE CONTROL FACTOR AND GENESIS OF LUOSHAN PB-ZN DEPOSIT IN LANPING,YUNNAN |
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| XU Xing-ye,HUANG Fa-mei,ZHANG Gui-yin,SU Tai-min,HUANG Lian-fei.THE ORE CONTROL FACTOR AND GENESIS OF LUOSHAN PB-ZN DEPOSIT IN LANPING,YUNNAN[J].Yunnan Geology,2013(4):421-423,416. |
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| Authors: | XU Xing-ye HUANG Fa-mei ZHANG Gui-yin SU Tai-min HUANG Lian-fei |
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| Institution: | Dali Branch of Geology ＆ Mineral Resources, Yunnan Exploration Institute of Geology ＆ Mineral Resources, Dali 671000) (2. Kunming Branch of Rapid Exploration ＆ Assessment, Yunnan Exploration Institute of Geology ＆ Mineral Resources, Kunming 650051 ) (3. Exploration Institute 2 of Geology ＆ Mineral Resources, Yunnan General Company of Geology ＆ Mineral Resources, Kunming 650051 ) |
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| Abstract: | The Pb - Zn deposit is in the ore - bearing limestone of Upper Triassic Sanhedong Formation Lower Member （T3s1 ） and nearly NS, NNE, NW fault fault fracture zone. A few are in the nearly EW joint fissure. It is a Pb - Zn multimetallic deposit of middle - low T hydrothermal type in genesis, which is controlled by horizon and structure with multiple metallogenetic stage and material source. |
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| Keywords: | Middle - Low T Hydrothermal Deposit Deposit Genesis Ore Control of Structure Luoshan Lanping Yunnan |
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