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碳酸岩中稀土元素富集成矿过程的隐藏线索

袁学银

岩石矿物学杂志2026,Vol.45Issue(2):365-377,13.
岩石矿物学杂志2026,Vol.45Issue(2):365-377,13.DOI:10.20086/j.cnki.yskw.2026.5131

碳酸岩中稀土元素富集成矿过程的隐藏线索

Hidden clues for rare earth element enrichment and mineralization in carbonatites:A review of mineralogical studies of carbocernaite and burbankite

袁学银1

作者信息

  • 1. 中国地质科学院矿产资源研究所,深地探测与矿产勘查全国重点实验室,北京 100037
  • 折叠

摘要

Abstract

Carbonatite-alkaline complex-associated rare earth element(REE)deposits are the principle sources of REEs.The enrichment and mineralization processes of REEs during such magmatic-hydrothermal systems are cur-rently the most highly debated issues in metallogenic studies.Due to the widespread occurrence of bastnäsite and monazite in nature,most studies are focused on the mineralogical and geochemical properties of REE phosphates and fluorcarbonates.Unfortunately,experiment results demonstrate that the solubilities of REE phosphates and flu-orcarbonates are insufficient for the formation of REE mineralizing fluids.By contrast,REEs also occur as Na-rich REE carbonate minerals in carbonatites,including carbocernaite and burbankite.These minerals are formed from some unique fluids,meanwhile easily altered during later hydrothermal processes,hence attracting limited research interests.However,according to the results from latest experiments,the transition from bastnäsite to carbocernaite via reacting with Na+and CO32-is the essential process that leads to the exceptional enrichment of REEs in aqueous liquids.Furthermore,REEs precipitate preferentially as carbocernaite or burbankite from Na-enriched carbonate fluids,and crystallization of bastnäsite occurs either during a relatively early stage where Na is insufficiently en-riched,or after Na precipitating substantially as alkaline silicate minerals during interaction with silicate wall rocks.These findings are consistent with REE occurring as burbankite in isolated systems(such as fluid inclusions),but as bastnäsite in carbonatite ore veins or other open systems,and indicate that such Na-rich REE carbonate minerals have clear implications for REE mobilization and mineralization processes.In this paper,we reviewed the crystal structures and chemical properties of carbocernaite and burbankite,and compared the occurrence of both minerals in carbonatite REE deposits to those in high pressure-temperature experiments,aiming to reveal the roles of such minerals during REE mobilization and mineralization processes,and provides clues for establishing a comprehensive REE metallogenic model in carbonatite systems.

关键词

碳铈钠石/黄碳锶钠石/碳酸岩/稀土矿床/富集成矿机理

Key words

carbocernaite/burbankite/carbonatite/rare earth element deposits/metallogenic mechanism

分类

天文与地球科学

引用本文复制引用

袁学银..碳酸岩中稀土元素富集成矿过程的隐藏线索[J].岩石矿物学杂志,2026,45(2):365-377,13.

基金项目

国家重点研发计划(2024YFC2909904) (2024YFC2909904)

国家自然科学基金项目(42522303) National Key Research and Development Program of China(2024YFC2909904) (42522303)

National Natural Science Foundation of China(42522303) (42522303)

岩石矿物学杂志

1000-6524

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