摘要
作者对363矿床的含矿岩体、构造和矿化特征进行详细的工怍,以大量宏观观察和微观测试的结果为依据,综合研究,提出矿床属热水沉积类型的设想。
The author has done detailed work on ore-bearing massif, structure and mineralization characteristics in ore deposit No.363. Through comprehensive study, based on extensive macroscopic observation and microscopic examination, an assumption is presented that the ore deposit is referred to hot water sedimentary type deposit.
出处
《铀矿地质》
CSCD
北大核心
1990年第2期77-84,共8页
Uranium Geology
关键词
铀矿床
矿床地质
矿化
成因
Uranium source, Structural stress, Hot water circulation
