| 670铀矿床地质特征及其成因 |
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| 引用本文： | 周家志.670铀矿床地质特征及其成因[J].华东地质学院学报,1992(1). |
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| 作者姓名： | 周家志 |
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| 作者单位： | 华东地勘局269队 |
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| 摘 要： | 本文提供了一个与火山侵入-隐爆角砾岩有直接成因联系的铀矿床实例。并从岩石学、岩石化学、同位素等方面介绍了成矿角砾岩的成岩特点及物质来源,阐述了与其有关的铀矿床的主要地质特征和矿床成因。
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| 关 键 词： | 铀矿床 地质特征 成因 |
THE GEOLOGICAL FEATURES AND ORIGINS OF NO 670 URANIUM DEPOSIT |
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| Zhou Jiazhi.THE GEOLOGICAL FEATURES AND ORIGINS OF NO 670 URANIUM DEPOSIT[J].Journal of East China Geological Institute,1992(1). |
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| Authors: | Zhou Jiazhi |
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| Abstract: | This paper gives an uranium deposit example which relates directly to volcanic intrusion dormant explosion breccia in origin. The rock-forming characteristics and materials source of mineralforming breccia are introduced in terms of petrology, petrological chemistry and isotopes. The main geological features and mineral deposit origins of uranium deposit related to it are stated. |
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| Keywords: | uranium deposit geological features cause of formation |
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