摘要
在分析伊犁盆地512铀矿床成矿水文地球化学背景的基础上,通过对水中铀存在形式、热力学、矿石物质组成和有机质分析,认为铀的还原沉淀是该矿床形成的主要水文地球化学作用。此外,铀的吸附作用也是重要的成矿作用。
The uranium reducting precipitation is known as the main uranium oreforming hydrogeochemistry for 512 uranium deposit by means of analysis of the uranium species, thermodynamics, ore composition and organic material concentration based on uranium oreforming hydrogeochemical setting of 512 deposit in Yili basin. In addition, adsorption of uranium is also an important mineralization.
出处
《地质找矿论丛》
CAS
CSCD
2003年第3期208-210,共3页
Contributions to Geology and Mineral Resources Research
基金
核工业科学基金项目(项目编号:Y7196R1801)资助。
关键词
铀还原沉淀
碳酸铀酰
512铀矿床
新疆
uranium reducting precipitation
hydrogeochemistry
512 Uranium deposit
Xinjiang
