摘要
纳米比亚湖山铀矿是一个特大白岗岩型铀矿,文章通过达马拉造山带构造特征,基底阿巴比斯杂岩体控制铀源,D型白岗岩发育直接控制铀矿化以及矿化的富集与后期热液改造有关等几个反面的阐述,研究了白岗岩的成矿规律。
The husab uranium deposit is a exceptional super-large alaskite-type uranium deposit in Namiba, Based on the tentonic characteristics of the Damala orogenic belt, The Abbabis basement rock controlled the uranium resource, The D-type alaskite directly controlled the Uranium mineralization and The enrichment of mineralization is related to the later hydro thermal transformation, The metallogenetic regulation of alaskite-type uranium deposit for Husab in Namibia has been summarized.
作者
李政
罗义
李宝新
LI Zheng;LUO Yi;LI Bao-xin(Sichuan Institute of Nuclear Geology,Chengdu 610000,China)
出处
《世界有色金属》
2017年第11期122-124,共3页
World Nonferrous Metals
关键词
达马拉造山带
D型白岗岩
热液
成矿规律
Damala orogenic belt
D-type alaskite
hydro thermal
metallogenetic regulation
