| 云南迪庆春都铜矿控矿地质条件 |
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| 引用本文： | 邹国富,罗书斌,吴昊,朱春蓉,李赛.云南迪庆春都铜矿控矿地质条件[J].云南地质,2009,28(4):403-408. |
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| 作者姓名： | 邹国富 罗书斌 吴昊 朱春蓉 李赛 |
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| 作者单位： | 中国有色金属工业昆明勘察设计研究院,云南昆明,650051 |
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| 摘 要： | 铜矿体赋存于印支期浅成-超浅成相的石英二长玢岩体内，具斑岩型矿床的蚀变特征，主要控矿因素为岩浆岩、岩浆侵位的地层、热液蚀变作用和构造裂隙等。是印支期甘孜-理塘洋向西俯冲造山晚期与超浅成斑（玢）岩密切有关的斑岩型铜矿床，矿区及外围具有较大的找矿潜力。
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| 关 键 词： | 斑岩型铜矿床 俯冲造山晚期 岛弧岩活动 印支期 云南迪庆春都 |
THE GEOLOGICAL CONDITIONS CONTROLLING ORE OF CHUNDU CU DEPOSIT IN DIQING,YUNNAN |
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| ZOU Guo-fu,LUO Shu-bin,WU Hao,ZHU Chun-tong,LI Sai.THE GEOLOGICAL CONDITIONS CONTROLLING ORE OF CHUNDU CU DEPOSIT IN DIQING,YUNNAN[J].Yunnan Geology,2009,28(4):403-408. |
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| Authors: | ZOU Guo-fu LUO Shu-bin WU Hao ZHU Chun-tong LI Sai |
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| Institution: | (Kunming Institute of Exploration ＆ Design, China Nonferrous Industry Company (Ltd), Kunming 650051 ) |
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| Abstract: | The Cu ore body of orefield exists in the Indosinian epizonal and super - epizonal quartz monzonite porphyrite, with the alteration characteristics of porphyry type ore deposit. The main ore - controlling factors are magmatic rock, strata of magma emplacement, hydrothermal alteration and structure fissure, etc. It is the porphyry type Cu deposit close in relation to super - epizonal porphyry （porphyrite） in late orogenic epoch of westward subduction of Indosinian Ganzi - Litang ocean. The prospecting potentiality is good in the orefield and surrounding area. |
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| Keywords: | Porphyry Type Cu Deposit Late epoch of Subduction Orogeny Magmatism of Island Arc Indosinian Chundu Diqing Yunnan |
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