ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
中国钒矿床类型、资源禀赋与开发利用现状
  
关键词:vanadium ore  deposit type  deposit genesis  metallogenic zone  development and utilization
基金项目:深地国家科技重大专项项目(编号: 2024ZD10020003);中国地质调查局地质调查项目(编号: DD20230040);科技基础资源调查专项课题(编号: 2022FY101703)
作者单位E-mail
戢兴忠 中国地质科学院矿产资源研究所 自然资源部成矿作用与资源评价重点实验室 jxz_cugb@126.com 
李强 中国地质科学院矿产资源研究所 自然资源部成矿作用与资源评价重点实验室 liqiangcags@163.com 
丁建华 中国地质科学院矿产资源研究所 自然资源部成矿作用与资源评价重点实验室  
陈其慎 中国地质科学院矿产资源研究所 自然资源部成矿作用与资源评价重点实验室  
张艳飞 中国地质科学院矿产资源研究所 自然资源部成矿作用与资源评价重点实验室  
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摘要:
Deposit Types, Resource Endowments, Development and Utilization of Vanadium Ore in China
      There are six types of vanadium deposits in China: sedimentary, magmatic, sedimentary metamorphic, volcanic, weathering, and hydrothermal types, among which the sedimentary and magmatic types of vanadium deposits play a leading role of the vanadium resources in China. Sedimentary vanadium deposits are mainly located at the northern margin of Tarim platform, northern and southeastern margins of Yangtze platform, while magmatic vanadium deposits are mainly located at the Emei Mountain large igneous province, Tarim large igneous province, and northern margin of the North China Craton. Vanadium ore is abundant in China, while the overall utilization rate is relatively low. Sedimentary vanadium ore is seldom used because of its low grade, high mining costs, and environmental protection policies. Vanadium-titanium magnetite of magmatic vanadium ores is the main raw material of vanadium. Strengthening the mining, technical research, and environmental protection of sedimentary vanadium ore, as well as continue to increase the comprehensive utilization of vanadium resources in magmatic vanadium-titanium magnetite are suggested as ways to realize green, high-quality, high-efficiency, and economic utilization of vanadium ore resources in China.
JI Xingzhong,LI Qiang,DING Jianhua,CHEN Qishen,ZHANG Yanfei.2025.Deposit Types, Resource Endowments, Development and Utilization of Vanadium Ore in China[J].Acta Geoscientica Sinica,46(5):965-978.
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