摘要
沽源-红山子钼多金属成矿带是我国北方钼矿主要赋存区域之一,研究区位于成矿带的南西段,具有较好的找矿潜力;本次研究通过对沽源-伦地区成矿带空间分布、含矿层位、围岩蚀变、成矿时代、成矿物质来源等特征的总结,分析区内钼矿床主要控矿因素,为该类矿床勘查提供理论指导。
The Gu Yuan-Hongshanzi molybdenum polymetallic mineral belt is one of the main molybdenum ore-bearing areas in northern China,and the study area is located in the southwest section of the mineral belt,which has good potential for mineral exploration.This study summarizes the spatial distribution,mineral-bearing strata,wall rock alteration,oreforming age,and source of ore-forming materials of the Gu Yuan-Lun area mineral belt,analyzes the main ore-controlling factors of the molybdenum deposits in the area,and provides theoretical guidance for the exploration of such types of deposits.
作者
王郅睿
张宗庆
王立新
张小朋
刘洋
WANG Zhi-rui;ZHANG Zong-qing;WANG Li-xin;ZHANG Xiao-peng;LIU Yang(School of Earth Science and Resources,Chang'an University,Xi’an 710054,China;Xi'an Center of Mineral Resources Survey,China Geological Survey,Xi’an 710100,China;Tianjin North China Geological Exploration Bureau,Nuclear Industry 247th Brigade,Tianjin 301899,China;Tianjin Huakan Nuclear Industry Resources Exploration and Development Co.,Ltd,Tianjin 301899,China)
出处
《世界有色金属》
2024年第18期88-90,共3页
World Nonferrous Metals
关键词
沽源-多伦地区
钼矿床
成矿地质特征
控矿因素
TheGuhuan-Duolun area
molybdenum deposit
ore-forming geological characteristics
controlling factors for ore formation
