| 浅析深部矿床和金属分带性成矿机理 |
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| 引用本文： | 文志成,桂发文,戴启冰.浅析深部矿床和金属分带性成矿机理[J].贵州工业大学学报(自然科学版),2008,37(4). |
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| 作者姓名： | 文志成 桂发文 戴启冰 |
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| 作者单位： | 贵州省地矿局一一五地质大队,贵州,贵阳,551400 |
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| 摘 要： | 大多数热液金属氧化物矿石形成于中地壳.深部水岩相互作用及其成矿流体性质决定了矿石的性质.从化学动力学角度阐述深部成矿和找矿的理论和实际问题.
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| 关 键 词： | 中地壳 金属分带性 周期性分布 自相似性 |
Analysis of Belts Mineralization Mechanism for Metallic and the Deep Orebody |
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| WEN Zhi-cheng,GUI Fa-wen,DAI Qi-bing.Analysis of Belts Mineralization Mechanism for Metallic and the Deep Orebody[J].Journal of Guizhou University of Technology(Natural Science Edition),2008,37(4). |
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| Authors: | WEN Zhi-cheng GUI Fa-wen DAI Qi-bing |
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| Institution: | WEN Zhi-cheng,GUI Fa-wen,DAI Qi-bing(No.5 Geological Team of Guizhou Bureau of Geology , Mineral Resources,Guiyang 551400,China) |
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| Abstract: | Most of hydrothermal metal oxide ore form on are in the middleal.That Deep-water interaction with rocks and its ore-forming fluid nature decide nature of the ore.The paper expatiate theoretical and practical problems of deep ore prospecting and Mineralization mechanism from chemical kinetics views. |
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| Keywords: | middle crustal metal donation periodic distributed self-similarity |
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