摘要
从区域地质特点分析以及从构造启动与矿液演化活动匹配的规律为依据,提出了在张光营-仙人嶂一线存在着一条较大的北北东向断裂构造,是矿田内第3条主成矿带。
By analyzing the regional geological characteristics and based on the law of tectonic movement matching with the ore-forming solution evolution, it is suggested that there would exist a larger NNE trending fault structure which is considered as the third main metallogenetic belt.
出处
《铀矿地质》
CAS
CSCD
北大核心
1993年第3期22-25,共4页
Uranium Geology
关键词
等间距
主成矿带
断裂带再活动
矿液演化
Equidistance, Main metallogenetic belt, Reactivation of the fault zone, Ore-forming solution evolution
