| 镇康芦子园铅锌矿床特征及成因 |
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| 引用本文： | 董文伟,陈少玲.镇康芦子园铅锌矿床特征及成因[J].云南地质,2007,26(4):404-410. |
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| 作者姓名： | 董文伟 陈少玲 |
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| 作者单位： | 云南地矿资源股份有限公司保山分公司,云南,保山,678000 |
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| 摘 要： | 芦子园铅锌矿产于镇康复背斜核部寒武系沙河厂组大理岩、板岩、片岩地层中，沿背斜轴部产生的断层及层间破碎带是主要的容矿构造，成矿物质来源于地层、酸性及基性岩浆热液，矿床成因为沉积-热液改造叠生型铅锌矿床。
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| 关 键 词： | 沉积热液改造 层位岩性控矿 中温叠生矿床 芦子园镇康云南 |
| 文章编号： | 1004-1885（2007）04-404-07 |
| 收稿时间： | 2006-08-07 |
THE CHARACTERISTICS & GENESIS OF LUZIYUAN PB-ZN DEPOSIT, ZHENKANG |
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| DONG Wen-wei,CHEN Shao-ling.THE CHARACTERISTICS & GENESIS OF LUZIYUAN PB-ZN DEPOSIT, ZHENKANG[J].Yunnan Geology,2007,26(4):404-410. |
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| Authors: | DONG Wen-wei CHEN Shao-ling |
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| Abstract: | The Luziyuan Pb- Zn deposit is occurred in the marble, slate and schist of Cambrian Shahechang Formation in the core of Zhenkang anticlinoria of Yunnan. And the fault and bedding fractured zone along the anticline axis are the main ore -bearing structures. The metallogenetic ele- ment originates from strata, thermal fluid of acidic and basic magma. The genesis of ore deposit belongs to the sedimentation -hydrothermal reformation superimpo sition type. |
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| Keywords: | Sedimentation - Hydrothermal Reformation Horizon - Litholo gical CharacterOre - Control Middle T Superimposition Ore Deposit Luziyuan Zhenkang |
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