| 西藏亚贵拉铅锌矿床地质特征及成因浅析 |
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| 引用本文： | 高明,张少波,岳国利.西藏亚贵拉铅锌矿床地质特征及成因浅析[J].沉积与特提斯地质,2010,30(2):97-102. |
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| 作者姓名： | 高明 张少波 岳国利 |
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| 作者单位： | 河南省地质调查院,河南,郑州,450001 |
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| 摘 要： | 本文通过对亚贵拉铅锌矿床地质特征、矿床地球化学特征等方面的分析,初步认为该矿床属于受层间构造破碎带和岩体接触带控制的热液充填-交代型脉状矿床,后期受到一定的构造改造,矿床的后生成矿特征显著。
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| 关 键 词： | 西藏 亚贵拉矿区 地质特征 矿床成因 |
Geology and genesis of the Yaguila lead-zinc deposit in Xizang |
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| GAO Ming,ZHANG Shao-bo,YUE Guo-li.Geology and genesis of the Yaguila lead-zinc deposit in Xizang[J].Sedimentary Geology and Tethyan Geology,2010,30(2):97-102. |
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| Authors: | GAO Ming ZHANG Shao-bo YUE Guo-li |
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| Institution: | (Henan Institute of Geological Survey,Zhengzhou 450001,Henan,China) |
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| Abstract: | The integration of geology and geochemistry of the Yaguila lead-zinc deposit in Xizang indicates that the lead-zinc deposit is assigned to the hydrothermal filling-metasomatic vein deposit of epigenetic origin,and controlled by interstratified structural fracture zone and orebody contact zone. |
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| Keywords: | Xizang Yaguila lead-zinc deposit geology genesis |
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