| 试论斑岩铀矿成矿系列 |
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| 引用本文： | 张彦春.试论斑岩铀矿成矿系列[J].铀矿地质,2002,18(5):264-272. |
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| 作者姓名： | 张彦春 |
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| 作者单位： | 中国核工业地质局290研究所,广东韶关,512026 |
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| 摘 要： | 本为作多年来在火山岩型铀矿领域的工作总结。章详细论述了斑岩铀矿成矿系列的特征，认为大部分火山岩型铀矿床的形成与火山活动晚期、最晚阶段的岩有着密切的关系。这些斑岩主要是花岗斑岩、霏细斑岩、石英斑岩。
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| 关 键 词： | 火山岩型铀矿床 斑岩成矿系列 成矿模式 火山活动 成矿作用 |
| 文章编号： | 1000-0685(2002)05-0264-09 |
| 修稿时间： | 2001年2月16日 |
Preliminary discussion on porphyry uranium metallogenic series |
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| ZHANG Yan,chun.Preliminary discussion on porphyry uranium metallogenic series[J].Uranium Geology,2002,18(5):264-272. |
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| Authors: | ZHANG Yan chun |
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| Abstract: | This paper is a summary of the research work of the author in the field of volcanic uranium deposits during last years. Characteristics of porphyry uranium metallogenic series are described in detail in the paper. It is suggested that the formation of most volcanic uranium deposits is closely associated with the porphyry of the late or the latest volcanism. Mostly, these are granite porphyry, felsite porphyry and quartz porphyry. |
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| Keywords: | volcanic type uranium deposit porphyry metallogenic series metallogenic model |
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