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湘东明月峰铀矿床位于湖南省东部株洲市境内,是我国重要的铀多金属南岭成矿带的重要铀矿床之一,处于区域性NNE-NE主干断裂附近及与其相伴生的二、三级断裂裂隙或向层间破碎带中,与华南陆块内部湘东北晚燕山期的区域构造线方向(胡瑞忠等,2007)一致。自上世纪50―70年代开始,许多地勘单位及科研工作者对此矿区的岩体、地质构造及铀矿化特征等方面做了许多的工作,铀矿主要产于此区印支期和燕山期岩体的内、外接触带中,并一直被视为外带型铀矿床,其矿化并非华南典
The Mingyuefeng uranium deposit in eastern Hunan Province is located in the territory of Zhuzhou City in the east of Hunan Province. It is one of the important uranium deposits of the important uranium-polymetallic Nanling metallogenic belt in China. It is located in the vicinity of the regional NNE-NE main fault and its accompanying secondary and tertiary Level fractures or inter-layer crustal zones are consistent with the regional tectonic line direction (Hu Ruizhong et al., 2007) of the late Yanshanian period in the northeastern Hunan Province of southern China. Since the 1950s and 1970s, many geological exploration units and researchers have done a lot of work on the rock mass, geological structure and uranium mineralization features of this mining area. Uranium deposits are mainly produced in the Indosinian and Yanshanian rock mass in the outer contact zone, and has been considered as a uranium ore belt, its mineralization is not South Code