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.
