安徽地质2025，Vol.35Issue(3)：193-196,202,5.
安徽庐枞矿集区何家大岭铁矿床铁氧化物微量元素特征及其指示意义
Geochemical characteristics and metallogenic implications of iron oxides and trace elements in the Hejiadaling iron deposit,Lu-Zong Ore Cluster,Anhui Province
摘要
Abstract
The Hejiadaling iron deposit,a representative porphyritic-type mineralization in the Lu-Zong ore cluster,exhibits vertical zoning from deep magnetite through hematite to shallow pyrite,with hematite predominating.Micro-area analysis reveals trace element partitioning in iron oxides:Mg,Ca,Al,Co and Ni demonstrate water-rock interaction signatures,Ti exhibits temperature-dependent behavior,while Mn and Zn reflect combined thermal,fluid-chemical and reaction-intensity controls.Vanadium distribution correlates with oxygen fugacity variations.Paragenetic minerals show negligible influence on iron oxide trace element signatures.The magnetite→hematite→pyrite transition sequence and hematite dominance confirm Hejiadaling's classification as an IOA-type deposit.关键词
庐枞矿集区/何家大岭/铁氧化物/微量元素Key words
Lu-Zong ore cluster/Hejiadaling deposit/iron oxides/trace element分类
天文与地球科学引用本文复制引用
张矿,刘一男..安徽庐枞矿集区何家大岭铁矿床铁氧化物微量元素特征及其指示意义[J].安徽地质,2025,35(3):193-196,202,5.基金项目
安徽省自然资源科技项目"安徽省典型玢岩铁矿床中钴的赋存状态及可利用性研究"(编号:2022-K-10)资助 （编号:2022-K-10）
