| 云南宝兴厂金多金属矿床成矿地质条件 |
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| 引用本文： | 王绍明,涂国府.云南宝兴厂金多金属矿床成矿地质条件[J].云南地质,2009,28(4):374-379. |
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| 作者姓名： | 王绍明 涂国府 |
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| 作者单位： | 武警黄金第10支队,云南昆明,650111 |
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| 摘 要： | 矿区金、铜、钼矿化与碱性斑岩相关，向阳组碎屑岩是主要矿源层及赋矿地层，北东向响水断裂控矿，近东西向次级断裂及层间断裂为储（容）矿构造。多种条件耦合成矿。
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| 关 键 词： | 金铜钼多金属 斑岩-构造蚀变型 构造岩浆控矿 次级构造容矿 云南弥渡宝兴厂 |
THE GEOLOGICAL CONDITIONS OF METALLOGENESIS OF BAOXINGCHANG AU MULTIMETALLIC DEPOSIT,YUNNAN |
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| WANG Shao-ming,TU Guo-fu.THE GEOLOGICAL CONDITIONS OF METALLOGENESIS OF BAOXINGCHANG AU MULTIMETALLIC DEPOSIT,YUNNAN[J].Yunnan Geology,2009,28(4):374-379. |
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| Authors: | WANG Shao-ming TU Guo-fu |
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| Institution: | ( Au Team 10 of Armed Police, Kunming 650111 ) |
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| Abstract: | In the orefield, the Au, Cu, Mo metallogeneses are related with the alkaline porphyry. The Xiangyang Formation clastic rocks are the main ore source bed and ore -beating strata. The NE Xiangshui fault is the ore -controlling fault. The ore -beating structure is the subsidiary fault in nearly EW and interlayer fault. The ore deposit results from the combination of many factors. |
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| Keywords: | Au - Cu - Mo Muhimetallic Deposit Porphyry--Structure Alteration Type Ore - Controlling of Structure--Magma Subsidiary Ore - Beating Structure Baoxingchang Midu Yunnan |
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