| 永平水泄铜钴矿控矿因素 |
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| 引用本文： | 杨宏城. 永平水泄铜钴矿控矿因素[J]. 云南地质, 2007, 26(4): 416-420 |
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| 作者姓名： | 杨宏城 |
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| 作者单位： | 云南有色地质310队,云南,大理,671005 |
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| 摘 要： | 水泄铜钴矿区地质条件较为复杂,控矿因素较多,通过分析认为主要受断层及岩性控制,地层初始富集,构造及区域变质作用提供通道及热源。水的循环、溶解作用形成热卤水成矿。
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| 关 键 词： | 麦初菁组碎屑岩 N-E向断裂系 蚀变次生变富 铜钴矿 水泄永平云南 |
| 文章编号： | 1004-1885（2007）04-416-05 |
| 收稿时间： | 2007-03-15 |
| 修稿时间： | 2007-03-15 |
THE ORE CONTROL FACTORS OF SHUIXIE CU-CO DEPOSIT IN YONGPING |
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| YANG Hong-cheng. THE ORE CONTROL FACTORS OF SHUIXIE CU-CO DEPOSIT IN YONGPING[J]. Yunnan Geology, 2007, 26(4): 416-420 |
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| Authors: | YANG Hong-cheng |
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| Abstract: | The geological conditions of Shuixie orefield are very complicated,with many ore control factors.According to the factor analysis, we think it is mainly controlled by the fault and lithological character,including the preliminary concentration in strata,channel and heat source provided by structure and regional metamprphism,deep circulation of water,hot brine formation by solution,etc. |
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| Keywords: | Clastic Rock of Maichuqing Formation NE Fault System Alteration Secondary Enrichment Cu-Co Deposit Shuixie Yongping |
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