| 对212铀矿床成矿作用的再认识 |
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| 引用本文： | 宋近发.对212铀矿床成矿作用的再认识[J].铀矿地质,1991,7(1):24-30. |
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| 作者姓名： | 宋近发 |
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| 摘 要： |
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| 关 键 词： | 铀矿 矿床 成矿作用 |
A NEW RECOGNITION ON METALLOGENESIS OF URANIUM DEPOSIT NO. 212 |
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| Song Jinfa.A NEW RECOGNITION ON METALLOGENESIS OF URANIUM DEPOSIT NO. 212[J].Uranium Geology,1991,7(1):24-30. |
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| Authors: | Song Jinfa |
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| Abstract: | Uranium deposit No.212 occurs at the margin of a Cenozoic continental basin, the formation of its mineralization has experienced four metallogenetic stages: early hydrothermal, syngenetic sedimentation,epigenetic concentration and late hydrothermal and is controlled by specific metallogenetic conditions. Metallogenetic characteristics depend on different portions of the deposit and different development of metallogenesis. |
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| Keywords: | Metallogenesis Syngenetic sedimentation Epigenetic concentration Hydrothermal superimposition |
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