| 万泉寺银金矿成矿作用分析 |
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| 引用本文： | 张阔,赵闯,牛树银.万泉寺银金矿成矿作用分析[J].吉林地质,2009,28(1):31-35. |
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| 作者姓名： | 张阔 赵闯 牛树银 |
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| 作者单位： | 石家庄经济学院,河北,石家庄,050031 |
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| 摘 要： | 万泉寺银金矿主要产于侏罗系白旗组二段地层中。其成矿作用主要为深部成矿物质随岩浆发生反重力迁移,最终通过较大断裂上升并于较大构造带中富集成矿。本文通过对该矿区成矿特征的阐述得出几点找矿标志,以便于对同类矿床的勘查提供参考。
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| 关 键 词： | 成矿作用 反重力迁移 万泉寺银金矿 找矿标志 |
Mineralization of Wanquansi Ag-Au deposit |
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| ZHANG Kuo,ZHAO Chuang,NIU Shu-yin.Mineralization of Wanquansi Ag-Au deposit[J].Jilin Geology,2009,28(1):31-35. |
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| Authors: | ZHANG Kuo ZHAO Chuang NIU Shu-yin |
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| Institution: | (Shijiazhuang Economic Institute, Shoiazhuang 050031, Hebei, China) |
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| Abstract: | Wanquansi Ag-Au deposit mainly occurred in the second strata, Jurassic Baiqi Formation. From the mineralization, as the magma antigravitational migration, the deep metallogenetic matter raised through large faults and hosted larger tectonic belt, finally, enriched mineralization. Based on the metallogenetic characteristics in the study area, we proposed some ore-hunting indicators in order to search for the same deposits for reference. |
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| Keywords: | mineralization antigravitational migration Wanquansi Ag-Au deposit ore-hunting indicator |
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