| 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。 |
| 关键词: 西藏 亚贵拉矿区 地质特征 矿床成因 |
| DOI： |
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| Geology and genesis of the Yaguila lead-zinc deposit in Xizang |
| GAO Ming, ZHANG Shao-bo, YUE Guo-li |
| (Henan Institute of Geological Survey, Zhengzhou 450001, Henan, China) |
| 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. |
| Key words: Xizang Yaguila lead-zinc deposit geology genesis |
