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赣中金滩岩体产铀花岗岩磷灰石地球化学特征及地质意义

刘龙 张树明 孟平虹 袁庚红 许谱林

铀矿地质2026,Vol.42Issue(5):695-709,15.
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铀矿地质2026,Vol.42Issue(5):695-709,15.DOI:10.3969/j.issn.1000-0658.2026.42.054

赣中金滩岩体产铀花岗岩磷灰石地球化学特征及地质意义

Geochemical Characteristics and Geological Significance of Apatite in Uranium-Bearing Granite of Jintan Pluton,Central Jiangxi

刘龙 1张树明 2孟平虹 1袁庚红 3许谱林1

作者信息

  • 1. 赣东学院,江西 抚州 344000
  • 2. 东华理工大学,江西 南昌 330013
  • 3. 江西省地质局第九地质大队,江西 吉安 343000
  • 折叠

摘要

Abstract

Jintan pluton is an Indosinian multi-stage and multi-phase composite pluton in central Jiangxi Province.It currently hosts the medium-sized Xiali uranium deposit and several uranium occurrences,including Xingjiazhou and Chouxi,and is therefore a uranium-bearing granitic pluton.In this paper,the garnet-bearing two-mica granite from Jintan pluton was selected for investigation.In situ major-and trace-element compositions of apatite were analyzed by Electron Probe Microanalysis(EPMA)and Laser Ablation Inductively Coupled Plasma Mass Spectrometry(LA-ICP-MS),aiming to constrain the petrogenesis of the granite and its implications for uranium mineralization.Our results show that,based on apatite geochemical parameters including REE distribution patterns,F/Cl,Sr/Mn,(Ce/Yb)N,Th/U,and Sr/Y ratios,the garnet-bearing two-mica granite is classified as S-type granite.The apatite is characterized by high F and low Cl contents,suggesting that the granite was derived from partial melting of continental crustal materials.The strongly negative Eu anomalies,weakly positive Ce anomalies,low SO ₃ contents,and high Mn contents of apatite reflect a low oxygen fugacity environment during magmatic evolution.The coupling of high degrees of fractional crystallization and low oxygen fugacity not only facilitated the crystallization and precipitation of uraninite at the magmatic stage,but also provided fundamental metallogenic conditions for the extraction of uranium by later hydrothermal activity.Comprehensive analysis indicates that the geochemical characteristics of apatite can effectively constrain the petrogenesis of the uranium-bearing granite and offer valuable geochemical proxies for improving our understanding of hydrothermal uranium mineralization mechanisms.

关键词

产铀花岗岩/磷灰石/地球化学/金滩岩体/赣中

Key words

uranium deposit host granite/apatite/geochemistry/Jintan pluton/central Jiangxi

分类

天文与地球科学

引用本文复制引用

刘龙,张树明,孟平虹,袁庚红,许谱林..赣中金滩岩体产铀花岗岩磷灰石地球化学特征及地质意义[J].铀矿地质,2026,42(5):695-709,15.

基金项目

赣东学院博士科研启动基金(编号:122000802)资助 (编号:122000802)

铀矿地质

1000-0658

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