| 镜铁山桦树沟铜矿床地质特征,成因及形成机制探讨 |
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| 引用本文： | 姚养利.镜铁山桦树沟铜矿床地质特征,成因及形成机制探讨[J].地质与勘探,2000,36(5):15-19. |
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| 作者姓名： | 姚养利 |
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| 作者单位： | 冶金工业部西北地质勘查局五队,酒泉,735000 |
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| 摘 要： | 介绍了镜铁山式铜矿床的地质特征，分析了其成因，并对其形成过程进行理论推导。认为该矿床为火山作用有关的中－低温热液改造层控矿床。
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| 关 键 词： | 地质特征 热液改造 层控铜矿床 镜铁山 |
DISCUSSION ON GEOLOGICAL CHARACTERISTICS, ORIGIN AND FORMATION PROCESSES OF THE HUASHUGOU COPPER DEPOSIT IN JINGTIE MOUNTAINS |
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| YAO Yang-li.DISCUSSION ON GEOLOGICAL CHARACTERISTICS, ORIGIN AND FORMATION PROCESSES OF THE HUASHUGOU COPPER DEPOSIT IN JINGTIE MOUNTAINS[J].Geology and Prospecting,2000,36(5):15-19. |
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| Authors: | YAO Yang-li |
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| Institution: | YAO Yang-li |
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| Abstract: | Geological characteistics of Jingtie Mountain's copper deposit was introduced. It's origin and formation processes are analysised. Huashugou copper deposit is believed to be a midle-low temperature hydrothermal reworked stratabound deposit relating to volcanic action. |
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| Keywords: | copper deposit geological characteristics hydrothermal rework stratabound deposit formation processes Jingtie Mountain |
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