摘要
华南地区白垩纪-古近纪断陷红盆发育,在空间和时间上与热液型铀矿床关系密切,尤其是花岗岩体外带上覆盆地型铀矿床。文章通过综合分析断陷红盆中铀矿床的成矿地质背景、矿床地质特征,结合区域大地构造演化,探讨了该类型铀矿床的成矿模式及找矿标志。
Faulted-down red basins of Cretaceous and Paleogene are extensively distributed in South China. The faulted-down red basins is close related to hydrothermal uranium deposits in time and apace. In this paper, the geological background and features of uranium deposits in faulted down red basins were analyzed synthetically. Prospecting indicators of this type uranium was discussed after studying their geotectonic evolution and the metallogenic model.
出处
《铀矿地质》
CAS
CSCD
2016年第2期99-103,127,共6页
Uranium Geology
基金
中国地质调查局“中国铀矿产地质总结”项目(编号:12120114039801)资助
关键词
花岗岩体外带上覆盆地型铀矿
断陷红盆
伸展构造
成矿模式
granite-peripheral uranium deposit in overlying basin
faulted down red basin
extensional tectonics
metallogenic model