| 试述华东南中新生代不整合面型铀矿床 |
| |
| 引用本文： | 陈祖伊,黄世杰.试述华东南中新生代不整合面型铀矿床[J].铀矿地质,1990,6(6):349-358. |
| |
| 作者姓名： | 陈祖伊 黄世杰 |
| |
| 摘 要： | 在华东南产出大量中新生代热液型铀矿床,其主要地质特征与世界上众所周知的元古代不整合型铀矿床十分相似。作者描述了这些热液型铀矿床的地质特征,讨论了其地质背景及可能的成矿机制,并认为,这类铀矿床可命名为中新生代不整合面型铀矿床。
|
| 关 键 词： | 不整合面型铀矿床 成矿机制 识别标志 |
ON MESO-CENOZOIC UNCONFORMITY-RELATED URANIUM DEPOSITS IN SOUTHEAST CHINA |
| |
| Chen Zuyi,Huang Shijie.ON MESO-CENOZOIC UNCONFORMITY-RELATED URANIUM DEPOSITS IN SOUTHEAST CHINA[J].Uranium Geology,1990,6(6):349-358. |
| |
| Authors: | Chen Zuyi Huang Shijie |
| |
| Institution: | Chen Zuyi;Huang Shijie |
| |
| Abstract: | A large amount of Meso-Cenozoic hydrothermal uranium deposits occurs in SoutheastChina, the main geological characteristics of which are quite similar to those of well-knownProterozoic unconformity-related uranium deposits in the world. The authors describe thegeological features of these hydrothermal uranium deposits, and discuss the geological settingand possible metallogenic mechanism, and conclude that these specific uranium deposits canbe nominated as Meso-Cenozoic unconformity-related uranium deposits. |
| |
| Keywords: | Unconformity-related uranium deposits Ore formation mechanism Recognition criteria |
| 本文献已被 CNKI 维普 等数据库收录！ |
|
