相山铀矿田611和6122矿床与34号矿床矿石建造特征对比  

COMPARISON OF ORE FORMATION CHARACTERISTICS OF URANIUM DEPOSIT NO.34 TO THOSE OF URANIUM DEPOSITS NO.611 AND 6122

作　　者：吴仁贵[1] 余达淦[1] 

机构地区：[1]华东地质学院,江西临川344000

出　　处：《铀矿地质》2000年第4期204-211,共8页Uranium Geology

基　　金：核科学基金!资助项目 (1/ 7196R180 2 ;96R180 0 3)

摘　　要：中国火山岩型铀矿床主要产于东南沿海一带 ,其矿石物质成分以单铀类型为主 ,但也存在一些复杂类型的矿床。本文旨就该类矿床中的铀及多元素建造类型列举了 34号矿床和相山矿田6 11,6 12 2等矿床进行具体对比。发现上述矿床在矿石物质成分上基本一致 ,表现为铀与钍、钇 (重稀土 )、钼、磷等构成铀多元素矿化类型。Volcanic type uranium deposits in China are mainly located in southeastern China with the predominant mono uranium subtype in ore composition. However, other types of uranium mineralization with complicated composition occur in this region too. This paper makes a specific comparison of ore composition of uranium deposits No.34 to that of uranium deposits No.611 and 6122, Xiangshan uranium ore field and discovers that these uranium deposits show basic identity in ore composition and belong to poly element mineralization type characterized by the association of uranium with thorium, yttrium (heavy REE), molybdenum and phosphorus.

关 键 词：矿石建造 火山岩型铀矿床 矿石矿物 

分 类 号：P619.140.4[天文地球—矿床学]