湖南省隆家铀矿控矿因素及成因探讨  

Exploring the Controlling Factors and Genesis of Longjia Uranium Deposit in Hunan Province

作　　者：杨清升 沈亚飞 许文力 

机构地区：[1]湖南省核地质调查所,湖南 长沙 [2]湖南省生态地质调查监测所,湖南 长沙

出　　处：《地球科学前沿（汉斯）》2024年第6期803-808,共6页Advances in Geosciences

摘　　要：隆家铀矿床位于雪峰山–摩天岭铀成矿带内,寒武系牛蹄塘组铀含量较高,为铀矿的形成提供了丰富的物质来源,矿区内褶皱及断裂构造发育,为铀的运移提供了良好通道和赋矿场所。本文在分析矿区地质特征、矿体特征及控矿因素的基础上,对矿床成因进行了探讨,认为矿床属碳硅泥岩型铀矿床。The Longjia uranium deposit is located in the Xuefengshan Motianling uranium mineralization belt. The Cambrian Niutitang Formation has a high uranium content, providing a rich material source for the formation of uranium deposits. Folds and fault structures are developed in the mining area, providing a good channel and ore-forming site for uranium migration. On the basis of analyzing the geological characteristics, ore body characteristics, and ore controlling factors of the mining area, this article explores the genesis of the deposit and believes that the deposit belongs to the carbon silicon mudstone leaching type uranium deposit.

关 键 词：隆家铀矿床 地质特征 控矿因素 矿床成因 

分 类 号：P61[天文地球—矿床学]