| 我国中新生代陆相盆地含铀沉积建造类型、特征及其研究意义 |
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| 引用本文： | 陈戴生.我国中新生代陆相盆地含铀沉积建造类型、特征及其研究意义[J].国外铀金地质,2012(3):135-141. |
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| 作者姓名： | 陈戴生 |
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| 作者单位： | 核工业北京地质研究院,中核集团铀资源勘查与评价技术重点实验室,北京100029 |
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| 摘 要： | 将我国中新生代陆相盆地含铀沉积建造类型划分为陆相暗色（灰色）含煤碎屑沉积建造、陆相红色（杂色）碎屑沉积建造及陆相红色含膏盐沉积建造3类，并概述其沉积特征。探讨了沉积建造研究在砂岩型铀矿科研及生产找矿方面的意义。
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| 关 键 词： | 中新生代陆相盆地 含铀沉积建造 区域构造演化 古气候变迁 |
The type, character and significance of uraniferrous formation in Meso-Cenozoic continental basin in China |
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| Authors: | CHEN Dai-sheng |
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| Institution: | CHEN Dai-sheng (CNNC Key Laboratory of Uranium Resources Exploration and Evaluation Technology, Beijing Research Institute of Uranium Geology, Beijing 100029, China) |
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| Abstract: | Uraniferrous formation in Meso-Cenozoic continental basin is divided into three types in this paper, continental grey coal bearing clastic rock formation, continental red （variegation） clastic rock formation and red continental gypsum bearing formation, and their features are summarized. The significances of the sedimentary formation in research and exploration are discussed for sandstone- hosted uranium deposits. |
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| Keywords: | Meso-Cenozoic continental basin uraniferrous sedinetary formation regional structuralevolution palaeoclimate change |
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