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粤西某稀土矿稀土元素赋存状态初探OACHSSCD

Preliminary Investigation on Occurrence State of Rare Earth Elements in a Rare Earth Ore in Western Guangdong

中文摘要英文摘要

稀土赋存状态是离子吸附型稀土矿成矿与开发的关键议题.粤西地区稀土资源丰富,但矿物学研究薄弱.以粤西某风化壳稀土矿为研究对象,采用偏光显微镜鉴定和硫酸铵常温浸出试验,研究稀土赋存状态.结果表明,含矿岩体中未检出独居石等独立稀土矿物,多处靶区矿石离子相浸出率为 64.00%~92.86%,整体较高.岩矿鉴定与浸出数据显示,稀土元素不形成独立晶质矿物,主要以可交换离子态吸附于黏土矿物表面,矿床类型属风化壳离子吸附型稀土矿.

Occurrence state of rare earth is the key issue for mineralization and development of ion adsorption rare earth ore.Rare earth resources are abundant in western Guangdong,but mineralogy research is weak.Taking a rare earth ore in a weathering crust in western Guangdong as the research object,the occurrence state of rare earth is studied by polarizing microscope identification and ammonium sulfate room temperature leaching test.The results show that no isolated rare earth minerals such as monazite are found in the ore-bearing rock mass,and the ion phase leaching rate of ores in multiple target areas is 64.00%to 92.86%,which is relatively high on the whole.Rock and ore identification and leaching data show that rare earth elements do not form independent crystalline minerals,and are mainly adsorbed on the surface of clay minerals in exchangeable ion state,and the deposit type belongs to weathering crust ion adsorption rare earth ore.

陈德进

广东省地质局肇庆地质调查中心,广东 肇庆 526060

天文与地球科学

稀土矿风化壳稀土元素赋存状态浸出率粤西

rare earth oreweathering crustrare earth elementsoccurrence stateleach ratewestern Guangdong

《中国资源综合利用》 2026 (9)

6-8,3

10.3969/j.issn.1008-9500.2026.09.002

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