| 杨志强,李占明,李俊芳,樊颖华,高金民,李琼.新疆东戈壁钼矿床地质特征及成矿热液作用阶段划分、矿物生成顺序研究[J].地质找矿论丛,2013,28(4):514-523 |
| 新疆东戈壁钼矿床地质特征及成矿热液作用阶段划分、矿物生成顺序研究 |
| Geological characteristics of East Gobi molybdenum deposit in Xinjiang and hydrothermal mineralization stages and mineral paragenesis in the deposit |
| 投稿时间：2013-01-11 |
| DOI：10.6053/j.issn.1001-1412.2013.04.003 |
| 中文关键词: 热液成矿过程 矿物生成顺序 斑岩型钼矿 东戈壁 东天山 新疆 |
| 英文关键词:hydrothermal metallization progress mineralparagenesis porphyry molybdenum deposit East Gobi eastern Tianshan Xinjiang |
| 基金项目: |
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| 中文摘要: |
| 新疆东戈壁斑岩型钼矿床是西北地区发现的第一个特大型钼矿床，矿床产于下石炭统浅变质碎屑岩夹火山岩中，位于雅满苏大断裂附近。文章通过分析含矿脉体之间的交切关系及生成先后顺序，将东戈壁钼矿成矿期热液作用划分为4个阶段；根据金属矿物之间的穿插、交代、共边关系，确定了矿物生成的先后顺序。 |
| 英文摘要: |
| East Gobi molybdenum deposit in Xinjiang is the first super-large deposit discovered in northwest China. It is located near the Yamansu fault and occurrs in low grade metamorphic Lower Carboniferous clastic rock intercalated with volcanic rocksl. According to cutting relation of ore veins hydrotrhermal mineralization in the deposit is divided into 4 stages and mineral paragenesus is determined on basis of cutting, replacement and edge share relation of the minerals. |
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