摘要
以邹家山矿床实测井温资料为基础 ,对矿床低温热水的分布规律、成因作了全面分析。采用将今论古的方法 ,结合铀成矿机理 ,探讨了古热水与铀成矿作用的关系 ,并预测邹家山矿床深部仍有较好的成矿远景。
Distribution and Genesis of low-thermal water in Zhoujiashan deposit are fully analysed on the basis of logging temperature data.With \!past inferred from present\' method and uranium mineralization mechanism,relationship between palaeothermal water and uranium mineralization is discussed,a metallogenetical prospect is hopefully predicted in the depth of zhoujiashan deposit.\;
出处
《华东地质学院学报》
2000年第1期24-27,共4页
Journal of East China Geological Institute
关键词
低温热水
铀矿化
邹家山
铀矿床
矿床成因
Low thermal water
Genesis
Uranium mineralization
Zhoujiashan deposit