摘要
本文通过热力学的计算方法,确定了测老庙盆地水中铀的存在形式,分析了铀在水中的迁移规律和沉淀条件。并应用饱和指数的找矿机理,对测老庙盆地的找矿前景提出了水文地球化学依据。
By dynamic calculation method. the existence form of uranium in the water of the Celaomiao Basin is determined) and the regularity of uranium migration and precipitation condition in the water is analysed. Moreover, hydrogeochemical basis for the prospecting potential of the Celaomiao Basin is presented on the basis of the prospecting mechanism of saturation index.
出处
《铀矿地质》
CSCD
北大核心
1990年第3期145-151,共7页
Uranium Geology
关键词
盆地
水
铀
存在形式
找矿
Existence form of uranium, Precipitating condition, Saturation index
