| 大理宝兴厂斑岩铜钼金矿成矿构造分析 |
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| 引用本文： | 周晓峰.大理宝兴厂斑岩铜钼金矿成矿构造分析[J].云南地质,2008,27(2):235-238. |
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| 作者姓名： | 周晓峰 |
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| 作者单位： | 武警黄金第十支队,云南,昆明,650111 |
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| 摘 要： | 三条大断裂形成三角形构造变形区，成为贯通岩石圈底部的通道。浅成斑岩多期入侵，以及内外接触带的破裂化和压扭破裂带的存在，为成矿创造有利条件。
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| 关 键 词： | 成矿前后断裂 幔-壳源浅成杂岩 铜钼金矿化 新生代斑岩 宝兴厂大理云南 |
AN ANALYSIS OF METALLOGENETIC STRUCTURE OF BAOXINGCHANG PORPHYRY CU - MO - AU DEPOSIT IN DALI |
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| ZHOU Xiao-feng.AN ANALYSIS OF METALLOGENETIC STRUCTURE OF BAOXINGCHANG PORPHYRY CU - MO - AU DEPOSIT IN DALI[J].Yunnan Geology,2008,27(2):235-238. |
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| Authors: | ZHOU Xiao-feng |
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| Institution: | ZHOU Xiao-feng ( Au Geological Team 10 of Armed Police, Kunming 650111 ) |
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| Abstract: | The triangular deformation area is formed by 3 grand faults, which becomes the channel to the bottom of lithosphere. The muhiperiodic intrusion of porphyry, clastation of inner and outer contact and the formation of pressure shear fault provide the advantageous conditions for the metallogenesis. |
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| Keywords: | Pre - Post - Metallogenesis Fault Mantle - Crust - Derived Epicomplex Cu- Mo - Au Metallogenesis Cenozoic Porphyry Baoxingchang Dab Yunnan |
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