| 保山镇康地块成矿条件及典型矿床成矿模式 |
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| 引用本文： | 董文伟. 保山镇康地块成矿条件及典型矿床成矿模式[J]. 云南地质, 2007, 26(1): 56-61 |
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| 作者姓名： | 董文伟 |
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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,保山,678000 |
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| 摘 要： | 镇康地块位于怒江断裂、龙陵-瑞丽断裂与柯街断裂、南汀河断裂之间。成矿地质条件优越,矿床属与岩浆热液有关的多期、多阶段、多矿质热液型多金属矿床。
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| 关 键 词： | 成矿条件 成矿模式 找矿模型 保山-镇康地场面 滇西南 |
| 文章编号： | 1004-1885（2006）01-056-07 |
| 收稿时间： | 2006-08-07 |
| 修稿时间： | 2006-08-07 |
THE METALLOGENETIC CONDITIONS AND TYPICAL MODEL IN BAOSHAN-ZHENKANG MASSIF |
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| DONG Wen-wei. THE METALLOGENETIC CONDITIONS AND TYPICAL MODEL IN BAOSHAN-ZHENKANG MASSIF[J]. Yunnan Geology, 2007, 26(1): 56-61 |
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| Authors: | DONG Wen-wei |
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| Affiliation: | Baoshan Branch, Yunnan Company ( Ltd |
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| Abstract: | The Baoshan-Zhenkang massif is between the Nujiang fault,Longling-Ruili fault and Kejie fault,Nantinghe fault.The geological conditions of metallogenesis is very good.The ore deposit belongs to the multistage,multiple metallogenetic hydrothermal multimetallic deposit related to the magmatic thermal fluid. |
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| Keywords: | Metallogenetic Conditions Metallogenetic Model Ore-Prospecting Model Baoshan-Zhenkang Massif Southwest Yunnan |
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