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江西赣县夏湖离子吸附型稀土矿成矿条件分析

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夏湖重稀土矿位于江西省赣县区,属离子吸附型稀土矿.研究表明,其成矿母岩主要为大埠复式花岗岩体中的黑云母二长花岗岩.根据其成分、结构和构造特征,可进一步划分为早期中粒斑状、中期中细粒少斑和晚期细粒含斑黑云母二长花岗岩.元素地球化学分析显示,黑云母二长花岗岩属高硅、富碱、贫钙镁、硅强烈过饱和的酸性花岗岩,由早至晚演化过程中,其基性组分逐渐减少,稀土元素含量升高,为夏湖重稀土矿的形成提供了重要物质来源.风化壳结构特征与矿体垂向变化特征研究表明,矿体主要产于燕山早期中粗粒黑云二长花岗岩风化壳的全风化层中,垂向上呈类似"绸带"状.
Analysis of metallogenic conditions of Xiahu ion-absorbing type rare earths deposit in Ganxian,Jiangxi Province
The Xiahu heavy rare earth ore is located in Ganxian District,Jiangxi Province,and belongs to the ion adsorption type rare earth ore.Research has shown that its ore-forming parent rock is mainly biotite monzogranite in the Dabu composite granite body.According to its composition,structure,and structural characteristics,it can be further divided into early medium grained porphyry,middle medium fine grained few spotted,and late fine grained biotite monzogranite.Element geochemical analysis shows that the biotite monzogranite belongs to an acidic granite with high silicon,rich alkali,poor calcium magnesium,and strong supersaturation of silicon.During its evolution from early to late,its basic components gradually decrease and the content of rare earth elements increases,providing an important material source for the formation of the Xiahu heavy rare earth deposit.The study on the structural characteristics of weathered crust and the vertical variation characteristics of ore bodies indicates that the ore bodies mainly occur in the fully weathered layer of the weathered crust of the early Yanshan coarse grained black cloud monzogranite,presenting a"silk ribbon"shape vertically.

ion adsorption typerare earth oremineralization conditionsGanxianJiangxi

张兴文、朱锦夫、刘宏

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江西省地质局第七地质大队,江西 赣州 341000

离子吸附型 稀土矿 成矿条件 赣县 江西

2024

世界有色金属
有色金属技术经济研究院

世界有色金属

影响因子:0.138
ISSN:1002-5065
年,卷(期):2024.(8)
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