| 云南永仁直苴斑岩型铜矿控矿条件及远景 |
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| 引用本文： | 辛荣.云南永仁直苴斑岩型铜矿控矿条件及远景[J].云南地质,2008,27(3):344-350. |
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| 作者姓名： | 辛荣 |
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| 作者单位： | 云南省有色地质楚雄勘查院,楚雄,675000 |
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| 摘 要： | NW向、近NS向断裂控制矿体展布，NW走向陡倾角断裂对成矿元素富集起主要作用，两组断裂交叉部位以及岩体内外接触带凹部是有利赋矿空间。铜、钼矿床具有多期、多阶段、多物质来源、多成矿作用的特点。
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| 关 键 词： | 斑岩型铜矿 两组断裂交汇 接触带凹部 构造控矿 直苴 永仁 云南 |
THE ORE CONTROL CONDITIONS AND PROSPECT OF ZHIJU PORPHYRY CU DEPOSIT IN YONGREN, YUNNAN |
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| XIN Rong.THE ORE CONTROL CONDITIONS AND PROSPECT OF ZHIJU PORPHYRY CU DEPOSIT IN YONGREN, YUNNAN[J].Yunnan Geology,2008,27(3):344-350. |
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| Authors: | XIN Rong |
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| Institution: | XIN Rong ( Chuxiong Nonferrous Exploration Institute of Yunnan, Chuxiong 675000 ) |
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| Abstract: | The ore -bearing rocks are quartz syenite porphyry, quartz syenite, granite porphyry and homfels, which belong to the transitional type between granite and syenite. The extension of ore body is controlled by the NW and nearly NS faults. The NW steep dip fault plays the main part in the concentration of metallogenetic element. The intersection of NW and NE faults and the concave part of inner and outer contact of rock body are the advantageous prospecting places. The Cu, Mo deposit is characterized by muhiphase, multiple material origin and metallogenesis. |
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| Keywords: | Porphyry Cu Deposit Intersection of Two Faults Concave Part of Contact Ore Control of Structure Zhiju Yongren Yunnan |
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