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稀土元素在岩浆和水热系统的实验岩石学和地球化学研究进展
引用本文:韦春婉,许成,付伟,易泽邦,李卓骐,石爱国,范朝熙,匡光喜.稀土元素在岩浆和水热系统的实验岩石学和地球化学研究进展[J].岩石学报,2022,38(2):455-471.
作者姓名:韦春婉  许成  付伟  易泽邦  李卓骐  石爱国  范朝熙  匡光喜
作者单位:北京大学地球与空间科学学院, 造山带与地壳演化教育部重点实验室, 北京 100871;北京大学地球与空间科学学院, 造山带与地壳演化教育部重点实验室, 北京 100871;桂林理工大学地球科学学院, 桂林 541006
基金项目:本文受国家自然科学基金项目(41825008、92162219)和广西自然科学基金项目(2020GXNSFGA297003)联合资助.
摘    要:稀土元素对绿色科技的发展具有至关重要的作用,随着世界范围内新兴技术的发展进程对稀土的需求日益提高,稀土矿床成矿机理的研究已经成为目前国际地学的研究热点.稀土元素分配行为的高温高压实验能够为研究稀土在岩浆和水热系统中的迁移、分异和沉淀机制提供有效制约,为了解稀土元素地球化学行为和稀土成矿作用提供重要的理论基础.本文总结了...

关 键 词:稀土元素  高温高压实验  分配系数  岩浆系统  热液系统  分异-富集-沉淀机制
收稿时间:2021/7/18 0:00:00
修稿时间:2021/10/10 0:00:00

Research advances in experimental petrology and geochemistry of rare earth elements in magmatic and hydrothermal systems
WEI ChunWan,XU Cheng,FU Wei,YI ZeBang,LI ZhuoQi,SHI AiGou,FAN ChaoXi,KUANG GuangXi.Research advances in experimental petrology and geochemistry of rare earth elements in magmatic and hydrothermal systems[J].Acta Petrologica Sinica,2022,38(2):455-471.
Authors:WEI ChunWan  XU Cheng  FU Wei  YI ZeBang  LI ZhuoQi  SHI AiGou  FAN ChaoXi  KUANG GuangXi
Institution:MOE Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, China;MOE Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, China;College of Earth Sciences, Guilin University of Technology, Guilin 540001, China
Abstract:With the development of new technologies and the increasing demands for rare earth elements (REEs) around the world, the metallogenic mechanism of rare earth deposits has become an international research hotspot. High-temperature and high-pressure experiments on the distribution behavior of rare earth elements can provide effective constraints for studying the migration, differentiation, and deposition mechanisms of rare earth elements in the magmatic and hydrothermal systems. The experiment results provide an important theoretical basis for the understanding of geochemical behavior of rare earth elements and the mineralization processes in the REE deposits. In this paper, we summarize the recent high-temperature and high-pressure experimental knowledge advances in the distribution behavior of rare earth elements in the magmatic and hydrothermal systems, including partial melting, liquid-liquid immiscibility, fractional crystallization, fluid-melt partitioning, as well as the migration, differentiation and precipitation mechanism of rare earth elements in the hydrothermal fluids. Finally, future work that enhances our understanding of rare earth elements migration and deposition mechanisms in magmatic and hydrothermal systems are briefly proposed.
Keywords:Rare earth element  High temperature-pressure experiment  Partitioning coefficient  Magmatic system  Hydrothermal system  Fractionation-enrichment-deposition mechanism
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