摘要
柯坪断隆的铀矿化主要产于北塔里木带中,共涉及5个矿化层位.研究结果认为,下古生界铀矿化属同生沉积叠加后生富集型,为后期热液流体提供了铀源,上古生界铀矿化可能与热液有关.
The north Tarim belt is the main uranium mineralization belt . There＇re five units, contain lower Cambrian Bulake formation , lower Ordovician , upper Devonian kezhiertage formation , upper Carboniferous and lower Permian Biyoulieti group . Lower Paleozoic formations which contain uranium supply materials to hot fluid and have deep influence on the concentration of other metal elements, main uranium spots contain Yinggang, Yaebake , Keping and so on. uranium mineralization has relation on the lower Permian＇s large scale basic magma activities.
出处
《新疆地质》
CAS
CSCD
北大核心
2010年第1期91-94,共4页
Xinjiang Geology
基金
核工业二一六大队集体工作成果
关键词
柯坪断隆
铀矿化
成因分析
Keping hump
Mineralization unit
Uranium mineralization
