沽源-多伦地区钼多金属成矿地质特征及控矿因素研究  

Research on the Geological Characteristics of Ore Formation and Ore-Controlling Factors of Volcanic Rock-Type Uranium Deposits in the Guyuan-Duolun Area

作　　者：王郅睿 张宗庆 王立新[3] 张小朋 刘洋[3,4] 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)

机构地区：[1]长安大学地球科学与资源学院,陕西西安710054 [2]中国地质调查局西安矿产资源调查中心,陕西西安710100 [3]天津华北地质勘查局核工业二四七大队,天津301899 [4]天津华勘核工业资源勘探开发有限公司,天津301899

出　　处：《世界有色金属》2024年第18期88-90,共3页World Nonferrous Metals

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.

关 键 词：沽源-多伦地区 钼矿床 成矿地质特征 控矿因素 

分 类 号：P618.51[天文地球—矿床学]