我国首次发现的多水钼铀矿  

FIRST DISCOVERY OF MOLURANITE IN CHINA

作　　者：张昭明[1] 束秀琴 

机构地区：[1]核工业北京地质研究院

出　　处：《铀矿地质》1995年第4期214-216,共3页Uranium Geology

摘　　要：多水钼铀矿属铀酰钼酸盐类矿物。我国首次发现的多水钼铀矿产于北方某火山岩型铀钼矿床的氧化带，为非晶质矿物，在显微镜下呈均质性，电子探针分析既含铀又含钼等是其主要特征。Moluranite is a mineral of uranyl molybdate group.The mineral discovered for the firsttime in China occurs in the oxidized zone of a volcanic uranium-molybdenum deposit in thenorthern part of China. The main characteristics of the mineral are that it is amorphous,isotropic under microscope and contains both uranium and molybdenum by electron-probeanalysis.

关 键 词：铀矿床 钼矿床 多水钼铀矿 

分 类 号：P619.14[天文地球—矿床学]