| 贵州水城青山铅锌矿床的成矿地质特征 |
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| 引用本文： | 欧锦秀. 贵州水城青山铅锌矿床的成矿地质特征[J]. 桂林工学院学报, 1996, 16(3): 277-282 |
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| 作者姓名： | 欧锦秀 |
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| 作者单位： | 桂林工学院资源工程系 |
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| 基金项目： | 中国右色金属工业总公司“八五’科研项目 |
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| 摘 要： | 矿体主要赋存在上石炭统马平群和二叠系下统梁山组中，呈似层状、透镜状产出．主要成矿元素为Ｐｈ，Ｚｎ，Ａｇ，铅加锌品位大于２２．２７％．成矿受地层层位、岩性、纵向断裂、层间裂隙控制，辉绿岩与成矿关系密切．
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| 关 键 词： | 铅锌矿床 成矿特征 控矿条件 地质特征 |
GEOLOGICAL CHARACTERISTICS ANDORE-CONTROL GEOLOGICAL CONDITIONS OFQINGSHAN LEAD-ZINC DEPOSIT,GUIZHOU |
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| Ou Jinxiu. GEOLOGICAL CHARACTERISTICS ANDORE-CONTROL GEOLOGICAL CONDITIONS OFQINGSHAN LEAD-ZINC DEPOSIT,GUIZHOU[J]. Journal of Guilin University of Technology, 1996, 16(3): 277-282 |
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| Authors: | Ou Jinxiu |
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| Abstract: | The ore bodies occurred in the stratoid and lens-like form with Mapping Group andLianshan Formation (C3mpP1l). The main ore-forming elements are Pb, Zn and Ag,and thegrade of Ph+Zn is above 22.27 percent.The ore bodies are controlled by stratalithology,longitudinal faulting and interlayer-gliding fault.There is close relationstip betwaeen diabaseand minerogenesis |
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| Keywords: | ead-zinc inerogenesis minerogenic characteristics ore-controlling conditions Guizhou |
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