摘要
从地质、水文地质两个方面入手,分析了柴达木盆地冷湖地区古近—新近系有利于可地浸砂岩型铀矿成矿的铀源,泥—砂—泥结构,补—径—排条件,及不利于可地浸砂岩型铀矿成矿与开发的构造因素。
This paper deals with uranium source, mud-sand - mud texture, hydrogeological conditions favorable to the U ore-formation in the Lower and Upper Tertiary in Lenghu, Qiadam and makes an approach to U ore potentiality.
出处
《四川地质学报》
2007年第2期104-106,共3页
Acta Geologica Sichuan
关键词
可地浸砂岩型铀矿
断陷盆地
层间氧化带
柴达木冷湖地区
in - situ leaching sandstone - type uranium deposit
faulted basin
interstratified oxidized zone
Leng-hu region, Qiadam
