摘要
通过对铀多金属矿成矿地质条件的探讨,总结了铀成矿基本规律,包括时控规律、空间分布规律、铀矿化类型及特征和控矿因素.其中强调指出,本区构造、地层和岩浆岩接触带三位一体联合控矿,而断裂构造作用是关键因素.在此基础上,进一步分析了找矿前景及找矿方向.
This paper discusses the ore-forming geological conditions of uranium polymetallic ore, summarizes the basic rules of uranium metallogenesis, control rules, including the time space distribution, type and characteristics of uranium mineralization and ore controlling factors. It indicated that, the tectonic, stratum and magmatite belt joint contact three-in-one ore controlling, and the fracture tectonic action is the key factor. On this basis, further analyzes the prospecting and prospecting direction.
出处
《湖南理工学院学报(自然科学版)》
CAS
2015年第2期74-80,共7页
Journal of Hunan Institute of Science and Technology(Natural Sciences)
关键词
铀多金属矿化
成矿地质条件
成矿规律
矿化类型
找矿方向
找矿前景
uranium polymetallic mineralization
the metallogenic geological conditions
metallogenic regularity
the mineralization type
prospecting direction
prospecting potential