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扬子陆块区东南缘碳硅泥岩型铀矿床与断陷红盆控矿机制
引用本文:张字龙,漆富成,何中波,李治兴,王文全,于金水. 扬子陆块区东南缘碳硅泥岩型铀矿床与断陷红盆控矿机制[J]. 国外铀金地质, 2012, 0(3): 125-129
作者姓名:张字龙  漆富成  何中波  李治兴  王文全  于金水
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
摘    要:扬子陆块区东南缘是碳硅泥岩型铀矿床的重要矿集区,其中沉积一外生改造型和沉积一热液叠加改造型铀矿床均分布在断陷红盆边缘或附近。通过红盆与碳硅泥岩型铀矿床分布规律的研究,提出了碳硅泥岩型铀矿床与红盆边缘断裂的沟通效应和控矿机制,旨在强调红盆在找矿实践中的权重。

关 键 词:碳硅泥岩型铀矿床  断陷红盆  控矿机制

Ore-controlling mechanism of down-faulted red basins over carbonaceous-siliceous-pelitic rock type uranium deposits at the southeastern margin of Yangtze continental block
ZHANG Zi-long,QI Fu-cheng,HE Zhong-bo,LI Zhi-xing,WANG Wen-quan,YU Jin-shui. Ore-controlling mechanism of down-faulted red basins over carbonaceous-siliceous-pelitic rock type uranium deposits at the southeastern margin of Yangtze continental block[J]. , 2012, 0(3): 125-129
Authors:ZHANG Zi-long  QI Fu-cheng  HE Zhong-bo  LI Zhi-xing  WANG Wen-quan  YU Jin-shui
Affiliation:(CNNC Key Laboratory of Uranium Resources Exploration and Evaluation Technology, Beijing Research Institute of Uranium Geology, Beijing 100029, China)
Abstract:One of the important ore-concentrated areas of carbonaceous-siliceous-pelitic rock type uranium deposits is the southeast continental margin of Yangtze plate. Sedimentary-exogenous transformation type and sedimentary-hydrothermal superimposed transformation type uranium deposits are always distributed at or near the edge of down-faulted red basins. By analyzing the relation of deposit distributions to down-faulted red basins, the connective effect and ore-controlling mechanism of carbonaceous-siliceous-pelitic rock type uranium deposits are proposed with marginal fractures of red basins in the paper.
Keywords:carbonaceous-siliceous-pelitic rock type uranium deposit  down-faulted red basins  ore-controlling mechanism
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