辽西大青山南部地段铀成矿地质条件分析  

Analysis of Uranium Metallogenic Conditions in the Southern Part of Mount Daqing Western Liaoning

作　　者：姜宝勇 李福 

机构地区：[1]辽宁省核工业地质二四二大队有限责任公司,辽宁 兴城

出　　处：《自然科学》2022年第2期165-174,共10页Open Journal of Nature Science

摘　　要：大青山南部地段位于辽宁省大青山铀成矿带内,其西部为著名的青龙铀矿田。区内断裂构造发育,岩浆活动强烈,围岩蚀变广泛,铀成矿地质条件良好。本文在综合分析研究该区多年铀矿找矿资料的基础上,结合区域地质背景,对区内铀成矿地质条件进行了初步分析,为区内进一步开展铀矿找矿工作提供参考依据。The southern part of Daqingshan is located in the Daqingshan uranium metallogenic belt in Liaoning Province, and the western part is the famous Qinglong uranium ore field. The area has developed fault structures, strong magmatic activity, extensive wall rock alteration and good uranium metallogenic geological conditions. Based on the comprehensive analysis and study of uranium prospecting data for many years in this area, combined with the regional geological background, this paper makes a preliminary analysis on the uranium metallogenic geological conditions in the area, so as to provide a reference basis for further uranium prospecting in the area.

关 键 词：大青山南部地段 铀成矿地质条件 铀矿化成因 

分 类 号：P619.14[天文地球—矿床学]