松辽盆地钱家店铀矿床层间氧化与铀成矿作用  

Discussion on the interlayer oxidation and uranium metallogenesis in Qianjiadian uranium deposit,Songliao Basin

作　　者：庞雅庆[1] 陈晓林[1] 方锡珩[1] 孙晔[1] 

机构地区：[1]核工业北京地质研究院,北京100029

出　　处：《铀矿地质》2010年第1期9-16,23,共9页Uranium Geology

摘　　要：通过系统的岩心观察、剖面对比和分析,笔者认为松辽盆地钱家店铀矿床的控矿层间氧化带主要由红色氧化砂岩与局部分布的黄色砂岩和灰白色砂岩组成。红色砂岩中含炭屑、黄铁矿、钛铁矿、菱铁矿,并遭强烈氧化,推断其原生色应主要为灰色,由后生氧化作用将其改造而呈现红色。层间氧化带的形态和展布特征主要受沉积相控制,后者也同时控制着铀矿化的产出。铀矿化在剖面上主要定位于红色氧化带减薄或尖灭部位,平面上主要分布于红色氧化带前锋线附近。Through systematic drill core observation, section contrast and analysis, it is proved that the ore-controlling interlayer oxidation zone of Qianjiadian uranium deposit is mainly composed by the red oxidized sandstone and locally distributed yellow and off-white sandstones. The red sandstone contains charcoal fragments, pyrite, ilmenite, siderite, which have been oxidized intensively, and it can be deduced that their original color was gray and became red due to the oxidization. The distribution of the oxidation zone is mainly controlled by the sedimentary facies, which also controll uranium metallization. The uranium orebodies mainly developed in the thinning or pinch parts of the red oxidation zone in section. On the plans, the uranium mineralization distributes near the front of the red interlayer oxidation zone.

关 键 词：钱家店铀矿床 层间氧化带 红色氧化砂岩 铀成矿 沉积相 

分 类 号：P612[天文地球—矿床学]