世界核地质科学2025，Vol.42Issue(6)：1239-1252,14.DOI:10.3969/j.issn.1672-0636.2025.06.008
柴达木盆地南缘乌图美仁地区狮子沟组砂岩型铀矿化特征及找矿方向
Characteristics and prospecting direction of sandstone type uranium mineralization in Shizigou formation in Wutumeiren area at the southern margin of Qaidam basin
摘要
Abstract
The discovery of profitable uranium boreholes in the Wutumeiren area indicates that the southern margin of the Qaidam basin has great potential for sandstone type uranium exploration.In order to further understanding the uranium mineralization conditions and prospecting potential in the Wutumeiren area,and clarify the direction of prospecting,this study systematically analyzed the uranium source,structure,sedimentary construction and alteration transformation,and systematically summarized the ore-forming elements of sandstone type uranium deposits in Shizigou formation of Wutumeiren area.It was believed that the Shizigou formation in Wutumeiren area on the southern margin of the basin had abundant uranium sources and formed a gentle anticline structure,developed braided river and braided river delta sand bodies,and with good redox conditions under a large monocline background.Combined with the characteristics of uranium mineralization,the uranium mineralization of the Shizigou Formation in the study area is believed a typical interlayer oxidation type uranium mineralization,controlled by sedimentary facies and structure.The western anticline belt can serve as a key area for the next step exploration.关键词
砂岩型铀矿/矿化特征/成矿模式/找矿方向/乌图美仁地区/柴达木盆地南缘Key words
sandstone-type uranium deposits/mineralization characteristics/metallogenic model/prospecting direction/Wutumeiren area/southern margin of Qaidam basin分类
天文与地球科学引用本文复制引用
SHAO Hengbo,CHEN Yunjie,CHEN Qing,KANG Ligang,XI Zhao,LAN Huaping,ZHANG Jin..柴达木盆地南缘乌图美仁地区狮子沟组砂岩型铀矿化特征及找矿方向[J].世界核地质科学,2025,42(6):1239-1252,14.基金项目
中国核工业地质局项目(编号:202519,202519-1,202519-2,202519-3)资助 Supported by China Nuclear Industry Geological Bureau Project(CNNC)(No.202519,202519-1,202519-2,202519-3) （编号:202519,202519-1,202519-2,202519-3）
