| 注册
首页|期刊导航|矿床地质|赣南大埠花岗岩体重稀土预富集机制

赣南大埠花岗岩体重稀土预富集机制

彭琳琳 王磊 杨斌 陈斌锋 李家桢 曾载淋 贺根文 马得青 杨雄涛

矿床地质2026,Vol.45Issue(4):807-824,18.
✕
矿床地质2026,Vol.45Issue(4):807-824,18.DOI:10.16111/j.0258-7106.2026.04.005

赣南大埠花岗岩体重稀土预富集机制

Pre-enrichment mechanism of heavy rare earth elements in Dabu granite pluton,southern Jiangxi Province:Evidence from zircon U-Pb ages and geochemistry

彭琳琳 1王磊 2杨斌 2陈斌锋 2李家桢 2曾载淋 2贺根文 2马得青 2杨雄涛2

作者信息

  • 1. 南京大学地球科学与工程学院,江苏南京 210023||江西省地质局,江西南昌 330036
  • 2. 江西省地质局第七地质大队自然资源部离子型稀土资源与环境重点实验室,江西赣州 341000
  • 折叠

摘要

Abstract

The Dabu granite pluton is located in the eastern section of the nearly E-W trending tectonic-magmatic belt in the Nanling Range.A world-class ion-adsorption type heavy rare earth element(HREE)deposit is developed in the pluton.At present,there is still controversy about the age of the main body of the Dabu pluton,and there is al-so a lack of systematic understanding of the initial enrichment mechanism of heavy rare earths.In this paper,the zircon U-Pb geochronology and whole rock geochemistry of the Dabu pluton were studied.The formation age of the main body of the Dabu pluton(biotite monzogranite)was(154.7±0.6)Ma,and the age of the complement(two-mica monzogranite)was(152.3±0.5)Ma,both of which were the products of early Yanshanian magmatic ac-tivity.Geochemical results show that the Dabu pluton is characterized by high silicon,rich alkali,poor iron and magnesium,relatively enriched Rb,Th,U,Ta,Pb elements and depleted Ba,Sr,P,Ti,Nb and other elements.The Zr/Hf(average 19.76)and Nb/Ta(average 5.23)ratios of the pluton are low,which belongs to the highly differ-entiated granite.With the crystallization and differentiation of magma,the Dabu pluton experienced the fractional crystallization of monazite,allanite and apatite,and the magmatic melt-fluid interaction gradually strengthened.HREE is increasingly enriched in the late two-mica monzogranite,which may be related to the fractional crystalli-zation of phosphorus-containing rare earth accessory minerals and the metasomatism of late F-rich fluids.The ear-ly-phase biotite granite(LREE/HREE ratio is low and rich in Y)and the late-phase two-mica granite or musco-vite granite of the highly fractionated granite are easy to form heavy rare earth ore after weathering.

关键词

重稀土矿床/锆石U-Pb定年/地球化学/高分异花岗岩/大埠

Key words

heavy rare earth deposit/zircon U-Pb dating/geochemistry/highly fractionated granite/Dabu

分类

天文与地球科学

引用本文复制引用

彭琳琳,王磊,杨斌,陈斌锋,李家桢,曾载淋,贺根文,马得青,杨雄涛..赣南大埠花岗岩体重稀土预富集机制[J].矿床地质,2026,45(4):807-824,18.

基金项目

本文得到国家重点研发计划项目(编号:2021YFC2901702)、江西省"科技+地质"联合计划项目(编号:2023KDG01006、2023KDG01007)和江西省地质局科技研究项目(编号:2022JXDZKJKY01)联合资助 (编号:2021YFC2901702)

矿床地质

0258-7106

访问量0
|
下载量0
段落导航相关论文