江西相山铀矿田构造控矿规律研究

对江西相山铀矿田内断裂构造格架及火山构造特征做了研究,认为相山火山盆地和断裂构造的成生与发育受永丰-抚州深断裂演化控制。从构造控矿作用看,相山铀矿田受大型中心式塌陷火盆控制,北部的EW向断裂带和中西部的EW向构造断陷带控制着矿田内的矿集带,NE向与EW向断裂构造复合部位控制了矿床的位置,密集成群的断裂裂隙带控制着铀矿体,使各矿床中的铀矿体呈群脉型。这些铀矿田地质构造特征及控矿规律对进一步找矿具有重要的指导意义。...

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Bibliographic Details
Published in地质与勘探 Vol. 51; no. 5; pp. 879 - 887
Main Author 窦小平 时燕华 吴赞华 熊超 万双双 孙崇波
Format Journal Article
LanguageChinese
Published 2015
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Summary:对江西相山铀矿田内断裂构造格架及火山构造特征做了研究,认为相山火山盆地和断裂构造的成生与发育受永丰-抚州深断裂演化控制。从构造控矿作用看,相山铀矿田受大型中心式塌陷火盆控制,北部的EW向断裂带和中西部的EW向构造断陷带控制着矿田内的矿集带,NE向与EW向断裂构造复合部位控制了矿床的位置,密集成群的断裂裂隙带控制着铀矿体,使各矿床中的铀矿体呈群脉型。这些铀矿田地质构造特征及控矿规律对进一步找矿具有重要的指导意义。
Bibliography:11-2043/P
DOU Xiao-ping, SHI Yan-hua , WU Zan-hua , XIONG Chao , WANG Shuang-shuang, SUN Chong-bo ( 1. Jiangxi Nuclear Industry Geological Bureau Testing Center, Nanchang,Jiangxi 330002; 2. Jiangxi Nuclear Industry Geological Bureau, Nanchang,Jiangxi 330046; 3. Key Laboratory of Tectonic Controls on Mineralization and Hydrocarbon Accumulation, Ministry of Land and Resources, Chengdu University of Technology, Chengdu,Sichuan 610059)
Xiangshan uranium orefield; fault structure; volcano-tectonic; tectonic ore-controlling
This study focuses on fault patterns and volcanic structures of the Xiangshan uranium ore-field in Jiangxi Province. The results suggest that the generation and development of the Xiangshan volcanic basin and faults are controlled by the three-step evolution of the Yongfeng-Fuzhou deep fault.From structural ore-controlling,the Xiangshan uranium ore-field is determined by large central-type collapse basins. The EW trending fault zone in north and the EW striking fault-depression belts in middle and
ISSN:0495-5331