| 东天山照壁山金矿床地质特征及成矿机制 |
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| 引用本文： | 陆彦,李保华,张斌. 东天山照壁山金矿床地质特征及成矿机制[J]. 成都理工大学学报(自然科学版), 1996, 0(2) |
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| 作者姓名： | 陆彦 李保华 张斌 |
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| 作者单位： | 成都理工学院地质学系，成都理工学院资源与经济系 |
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| 摘 要： | 照壁山金矿床位于东天山地区的红柳河构造带中，为产于华力西早期的照壁山黑云母花岗岩体中的浅成、中低温石英脉型金矿，成矿时期为新生代（喜马拉雅期）。
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| 关 键 词： | 东天山，石英脉型金矿，新生代成矿 |
GEOLOGICAL CHARACTERISTIC AND FORMATION-MECHANISM OF THE ZHAOBISHAN GOLD DEPOSIT IN THE EASTERN REGION OF TIANSHAN MOUNTIAINS |
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| Lu Yan, Li Baohua, Zhang Bin. GEOLOGICAL CHARACTERISTIC AND FORMATION-MECHANISM OF THE ZHAOBISHAN GOLD DEPOSIT IN THE EASTERN REGION OF TIANSHAN MOUNTIAINS[J]. Journal of Chengdu University of Technology: Sci & Technol Ed, 1996, 0(2) |
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| Authors: | Lu Yan Li Baohua Zhang Bin |
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| Abstract: | The Zhaobishan gold deposit is located in the Hongliuhe structural belt in the eastern region of Tianshan Mountiains. It is a hypergene, medium-low temperature quartz vein type gold deposit located in the granite of the early Variscan orogeny. Its mineralization period is Cenozoic Era. |
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| Keywords: | eastern region of Tianshan Mountains quartz vein type gold deposit Cenozoic mineralization |
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