赣西北修水地区碳硅泥岩型铀矿化特征及成矿模式分析  

An Analysis of Characteristics and Metallogenic Model on Carbon Siliceous Mudstone Type of Uranium Mineralization in Xiushui Area, Northwestern Jiangxi Province

作　　者：关显东 赖胜[1,2] 张文东 李秉书 苏特 王铂云 裴晓宇 李彭 GUAN Xiandong;LAI Sheng;ZHANG Wendong;LI Bingshu;SU Te;WANG Boyun;PEI Xiaoyu;LI Peng(College of Earth Sciences, Guilin University of Technology, Guilin, Guangxi 541000, China;Guangzhou Municipal Engineering Design and Research Institute, Guangzhou, Guangdong 510000, China;Beijing Resrarch Institute of Uranium Geology, Beijing 100029, China;The Fifth Detachment of CAPF, Xi'an 710100, China)

机构地区：[1]桂林理工大学地球科学学院,广西桂林541000 [2]广州市市政工程设计研究总院,广东广州510000 [3]核工业北京地质研究院,北京100029 [4]武警黄金第五支队,陕西西安710100

出　　处：《中国锰业》2019年第1期51-54,共4页China Manganese Industry

摘　　要：修水地区位于修水—宁国—开化碳硅泥岩成矿带西端,处于区域铀成矿的有利部位,是我国南方典型碳硅泥岩型铀矿集中区。在前人研究成果综合分析和开展野外地质调查的基础上,通过对修水地区多处碳硅泥岩型铀矿床资源调查评价工作,分析厘定并总结了修水地区碳硅泥岩型铀矿化特征及成矿模式,为下一步工作提供理论依据。Xiushui area is located in western end of Xiushui-Ningguo-Kaihua carbonaceous siliceous mudstone metallogenic belt, which is a favorable site for uranium mineralization in the region. It is a typical uranium deposit in the south of China. On the basis of comprehensive analysis of previous research results and field geological survey, this paper makes an analysis of the characteristics of uranium mineralization and metallogenic model of carbon siliceous mudstone type in Xiushui area. It provides a theoretical basis for the next work through the investigation and evaluation of the resources of carbon and silicon mudstone type uranium deposits in Xiushui area.

关 键 词：铀矿 矿化特征 成矿模式 

分 类 号：P618[天文地球—矿床学]