甘肃敦煌塔水井南钒矿矿体特征及成因探析  

Analysis of the Characteristics and Genesis of the South Vanadium Mine in Tashuijing,Dunhuang,Gansu Province

作　　者：李作鹏[1] LI Zuo-peng(The Third Geological and Mineral Exploration Institute of Gansu Bureau of Geology and Mineral Resources,Lanzhou 730050,China)

机构地区：[1]甘肃省地矿局第三地质矿产勘查院,甘肃兰州730050

出　　处：《世界有色金属》2023年第20期93-95,共3页World Nonferrous Metals

摘　　要：敦煌市塔水井南钒矿位于中国甘肃省敦煌市,作为中国西部地区的一处重要矿产地,其地质矿产特征及矿床成因一直备受学者和矿产资源开发者的关注。这一地区拥有丰富的钒矿资源,对于满足国内有色金属产业和高科技领域的需求至关重要,同时也在地质学、矿产资源开发和环境保护等领域具有重要意义。本论文旨在深入研究敦煌市塔水井南钒矿的地质矿产特征及矿床成因,以揭示其独特之处,为资源的可持续开发和生态环境的保护提供科学支持。通过详细的地质调查、矿物学分析、地球化学探讨以及先进的矿床成因研究,探析这一地区的地质形成过程、矿床类型及其形成机制.The Tashuijing South Vanadium Mine in Dunhuang City,Gansu Province,China is an important mining area in western China.Its geological and mineral characteristics and genesis have always been of great concern to scholars and mineral resource developers.This region has abundant vanadium ore resources,which are crucial for meeting the needs of the domestic non-ferrous metal industry and high-tech fields.It is also of great significance in fields such as geology,mineral resource development,and environmental protection.This paper aims to conduct in-depth research on the geological and mineral characteristics and genesis of the Tashuijing South Vanadium Mine in Dunhuang City,in order to reveal its uniqueness and provide scientific support for the sustainable development of resources and the protection of the ecological environment.Through detailed geological investigation,mineralogical analysis,geochemical exploration,and advanced research on the genesis of mineral deposits,this study aims to explore the geological formation process,types of mineral deposits,and their formation mechanisms in this region.

关 键 词：塔水井南钒矿 矿体特征 成因探析 

分 类 号：P618.61[天文地球—矿床学]