504铀矿床中硒的分布特征  

THE DISTRIBUTION FEATURES OF SELENIUM IN URANIUM DEPOSIT NO. 504

作　　者：陈露明[1] 张启发[1] 

机构地区：[1]贵州科学院

出　　处：《铀矿地质》1996年第2期91-94,共4页Uranium Geology

基　　金：国家自然科学基金

摘　　要：５０４铀矿床是一个铀－汞－钼多金属矿床，其中硒达到了综合利用指标，硒与铀密切正相关，并分布在各类铀矿体中。硒主要以硒化物矿物形式产出，矿床中还发现了新的硒矿物—硒锑矿。The uranium deposit No. 504 is a U-Hg-Mo polymetallic deposit. Selenium content in this deposit reaches the index of comprhensive utilization. A clear positive correlation is observable between Se and U. Selenium is distributed in different kinds of uranium ore body,and occurs mainly in the form of selenide minerals. A new selenium mineral-Antimonselite was also found in the uranium deposit No. 504

关 键 词：分布特征 铀矿床 硒 

分 类 号：P619.140.4[天文地球—矿床学]