| 刚果(金)DIMMA铜钴矿床地质特征及成因分析 |
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| 引用本文： | 刘运纪,王纪昆,张泰.刚果(金)DIMMA铜钴矿床地质特征及成因分析[J].地质找矿论丛,2011,26(4):446-452. |
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| 作者姓名： | 刘运纪 王纪昆 张泰 |
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| 作者单位： | 天津华北地质勘查总院,天津,300171 |
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| 摘 要： | DIMMA铜钴矿区位于著名的刚果（金）-赞比亚卢菲利褶皱弧铜钴矿带的北西端。DIMMA铜钻矿床的形成与成岩期的火山活动、同生断裂活动有关，并受后期造山过程中的褶皱、断裂和变质作用的改造和次生富集，形成多成因多重控制的铜钴矿床。
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| 关 键 词： | DIMMA铜钻矿 矿床特征 成矿流体 层控矿床 卢菲利褶皱带 刚果（金） |
| 收稿时间： | 2010/11/19 0:00:00 |
| 修稿时间： | 2011/9/14 0:00:00 |
Characteristtics of Dimma Cu-Co deposit in Congo-Kinshasa and analysis on its genesis |
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| LIU Yun-ji,WANG Ji-kun and ZHANG Tai.Characteristtics of Dimma Cu-Co deposit in Congo-Kinshasa and analysis on its genesis[J].Contributions to Geology and Mineral Resources Research,2011,26(4):446-452. |
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| Authors: | LIU Yun-ji WANG Ji-kun and ZHANG Tai |
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| Institution: | (Tianjin North China Geological Exploration General Institute,Tianjin 300171,China) |
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| Abstract: | Dimma Cu-Co deposit is located in the northwest end of Cu-Co ore belt in Luffilian fold arc at boundary between Congo（Kinshasa） and Zambia. It is related to volcanism and syn-sedimentary faulting and reworked by folding ,fracturing, metamorphism and secondary enrichment in late orogenic process.. Therefore, it is a polygenous Cu-Co deposit controlled by multi-factors. |
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| Keywords: | Dimma Cu-Co deposit characteristics of Dimma Cu-Co deposit ore fluid stratobound ore deposit Luffilian fold belt Congo-Kinshasa |
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