首页|黔北华尖铝土矿及含铝岩系中关键金属地质特征与成因探讨

黔北华尖铝土矿及含铝岩系中关键金属地质特征与成因探讨

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以正安县安场镇华尖铝土矿床作为研究对象,采用地质填图,稀疏地表工程槽探,深部工程钻探揭露和样品测试分析等手段,研究了区内的大竹园组铝土矿及伴生锂资源的矿床地质特征.研究结果表明,铝土矿及含铝岩系关键金属Li都赋存于大竹园组含铝岩系中上部,矿体呈层状、似层状产出;铝土矿主要在研究区中部以北富集,含铝岩系厚度变化与铝土矿及伴生元素Li的富集呈正相关,当厚度小于3m时,一般无矿;Li在致密状和碎屑状铝土矿(岩)中含量通常较高,少量在豆鲕状铝土岩,一般土状铝土矿中则不富集;Al2O3和Li的富集作用具耦合关系,当Al2O3含量少于55%时,Li的富集与之呈正相关,当含量≥60%时则不含锂矿;Li含量与SiO2相关性不明显,Li含量较高的矿一般Fe2O3较低.
Geological Characteristics and Genesis of Key Metals in Huajian Bauxite and Aluminium-bearing Rock Series in Northern Guizhou Province
Taking the Huajian bauxite deposit in Anchang Town,Zheng'an County as the research object,the geological characteristics of the bauxite deposit and associated lithium resources in Dazhuyuan Formation are studied by geological mapping,sparse surface engineering trough exploration,deep engineer-ing drilling and sample testing and analysis.The results show that both bauxite and Li,the key metal of alu-minum-bearing rock series,exist in the middle and upper part of aluminum-bearing rock series of Dazhuyu-an Formation.Bauxite is mainly enriched in the north of the middle of the study area,and the thickness change of Al-bearing rock series is positively correlated with the enrichment of bauxite and associated ele-ment Li.When the thickness is less than 3 m,there is generally no ore.The content of Li is usually high in dense and clastic bauxite(rock),and a small amount in bean oolitic bauxite,but not in general earthy baux-ite.The concentration of Al2O3 and Li has a coupling relationship.When the content of Al2O3 is less than 55%,the concentration of Li is positively correlated with it,and when the content is great than or equal to 60%,there is no lithium ore.The correlation between Li content and SiO2 is not obvious,and Fe2O3 ores with higher Li content is generally lower.

bauxiteLigeological characteristicsgenesis of deposit

袁孝刚、石再平、王永健、杨仕江、黄忠洪

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贵州省有色金属和核工业地质勘查局三总队

铝土矿 Li 地质特征 矿床成因

2024

现代矿业
中钢集团马鞍山矿山研究院有限公司

现代矿业

影响因子:0.33
ISSN:1674-6082
年,卷(期):2024.40(7)