| 库布苏金矿地质特征及成矿条件分析 |
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| 引用本文： | 高怀忠,张旺生.库布苏金矿地质特征及成矿条件分析[J].新疆地质,1998(2). |
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| 作者姓名： | 高怀忠 张旺生 |
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| 作者单位： | 中国地质大学!武汉430074 |
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| 基金项目： | 国家“305”项目!85 - 90 2 - 0 3- 0 2研究成果 |
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| 摘 要： | 库布苏金矿是东准噶尔地区发现的破碎带蚀变岩型金矿。该矿产于陆缘火山岩浆弧区 ,成因与强应变构造带及浅成、超浅成岩脉有关 ,成矿流体为高温近中性溶液 ,矿体受断裂破碎带控制
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| 关 键 词： | 库布苏 强应变构造带 成矿条件 金矿 |
GEOLOGICAL CHARACTERISTICSAND METALLOGENIC CONDITION OF KUBUSU GOLD DEPOSIT |
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| Gao Huaizhong,Zhang Wangsheng.GEOLOGICAL CHARACTERISTICSAND METALLOGENIC CONDITION OF KUBUSU GOLD DEPOSIT[J].Xinjiang Geology,1998(2). |
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| Authors: | Gao Huaizhong Zhang Wangsheng |
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| Abstract: | Kubusu gold deposit is of alteration type discovered in the fracture zones of east Junggar region. The deposit occurs at volcanomagmatic arc regions of continental margin,genetically related with high- strained structural zones and hybabyssal- ultrabyssal veins.The metallogenic fluid is nearly intermediate high- temperature solution.The ore body is controlled by fracture zones. |
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| Keywords: | Kubusu high- strained structural zone metallogenic condition gold deposit |
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