| 广西贵港—平南地区铅锌矿带地质特征及找矿方向 |
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| 引用本文： | 伍磊.广西贵港—平南地区铅锌矿带地质特征及找矿方向[J].矿产与地质,2001,15(5):329-334. |
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| 作者姓名： | 伍磊 |
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| 作者单位： | 广西有色地质勘查总院 |
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| 摘 要： | 广西贵港－平南地区分布有华南大型－超大型铅锌矿成矿的有利层位，北东向两条深断裂具有多期活动性，泥盆系沉积盖层中下部第一层碳酸盐岩与成矿关系密切。具有较广阔的找矿前景。主要铅锌矿类型有热水沉积＋构造热液迭加改造型、复合叠加型。
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| 关 键 词： | 铅锌矿床 地质特征 找矿方向 广西 碳酸盐岩 成矿作用 找矿前景 |
| 文章编号： | 1001-5663(2001)05-0329-06 |
| 修稿时间： | 2001年4月11日 |
GEOLOGICAL CHARACTER OF GUIGANG-PINGNAN LEAD-ZINC ORE ZONE OF GUANGXI AND ITS PROSPECTING DIRECTION |
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| WU Rui.GEOLOGICAL CHARACTER OF GUIGANG-PINGNAN LEAD-ZINC ORE ZONE OF GUANGXI AND ITS PROSPECTING DIRECTION[J].Mineral Resources and Geology,2001,15(5):329-334. |
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| Authors: | WU Rui |
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| Abstract: | The strata favorable for south china great gigantic type Lead Zinc ores' formation occur in Guigang pingnan distrct, Guangxi. Two NE trend deep rooted faults show multi period activity. The mineraliation is closely related to the first layer carbonate rocks of middle lower part of devonian system sedimentary mantle which have great potential for prospecting. The main Lead Zinc deposit type include hydrothermal sedimentation plus structure hydrothermal superimposed alteration type and complex superimposition type. |
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| Keywords: | Lead Zinc deposit Geologic character Prospecting direction |
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