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作 者:Xibin Lu Jianghao Bai Feng Ye Gangjian Wei
机构地区:[1]State Key Laboratory of Isotope Geochemistry,CAS Center for Excellence in Deep Earth Science,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou,510640,China [2]Key Laboratory of Marine Mineral Resources,Ministry of Natural and Resources,Guangzhou,511458,China [3]University of Chinese Academy of Sciences,Beijing,100049,China
出 处:《Journal of Earth Science》2024年第6期2129-2132,共4页地球科学学刊(英文版)
基 金:supported by the National Natural Science Foundation of China(Nos.92358301,42403001);the Key Laboratory of Marine Mineral Resources,Ministry of Natural and Resources,Guangzhou(No.KLMMR-2022-G08);China National Postdoctoral Program for Innovative Talents(No.BX20240377);China Postdoctoral Science Foundation(No.2023M743501);Director's Fund of Guangzhou Institute of geochemistry,CAS(No.2023SZJJ-1)。
摘 要:0 INTRODUCTION Rare earth elements(REEs)are integral to geochemical tracing systems due to their unique geochemical properties.Their distribution patterns,fractionation,anomalies,and radiogenic isotope characteristics have been extensively applied in various disciplines,including planetary science,marine science,environmental science,and economic geology.REEs possess multiple stable isotopes,whose distinctive signatures further augment the effectiveness of geochemical tracing.
关 键 词:GEOCHEMICAL EARTH ISOTOPE
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