中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Nb and Ta intracrustal differentiation during granulite-facies metamorphism: Evidence from geochemical data of natural rocks and thermodynamic modeling

文献类型:期刊论文

作者Huang, Guangyu2; Chen, Yi2; Guo, Jinghui2; Palin, Richard1; Zhao, Lei2
刊名AMERICAN MINERALOGIST
出版日期2022-11-25
卷号107期号:11页码:2020-2033
关键词Nb Ta granulite partial melting forward modeling ultrahigh temperature rutile High-Grade Metamorphism Crustal Melting and Granite Magmas
ISSN号0003-004X
DOI10.2138/am-2022-8260
英文摘要Both continental crust and depleted mantle are characterized by subchondritic Nb/Ta, leading to a mass imbalance when compared to the bulk Earth. Even though several potential high-Nb/Ta reservoirs in Earth's core and undepleted mantle have been proposed, little attention has been given to those in the crust. Here we present bulk-rock and rutile geochemical data for samples from a lower crustal pelitic granulite, North China Craton, which exhibit systematic variation in their Nb and Ta contents. High-temperature (HT) and ultrahigh-temperature (UHT) granulite residues exhibit Nb/Ta ratios that are close to chondritic and subchondritic, respectively, whereas leucosomes from UHT granulite mostly have suprachondritic Nb/Ta. These variations are best explained via competition for Nb and Ta between biotite and rutile during metamorphism, although initial bulk-rock Nb/Ta values also have an effect. As biotite preferentially incorporates Nb over Ta, the early stages of biotite dehydration melting produce a high-Nb/Ta residue and a low-Nb/Ta melt; however, geochemical modeling suggests that once biotite is depleted, the Nb/Ta ratio of the system is instead controlled by rutile growth, which promotes the formation of a lower Nb/Ta residue and a higher Nb/ Ta melt, even though the volume of melt produced at this stage may be small. We propose that in situ and in-source leucosomes and leucocractic veins in UHT terranes may retain a high-Nb/Ta geochemical signature. However, residual crustal-derived A2-type granites that experience significant fractionation of Nb- or Ta-bearing minerals during crystallization or contamination from other low-Nb/Ta sources cannot retain this high-Nb/Ta ratio, even though these ratios are generally higher than that of S-type granites. Anhydrous partial melting of metapelite can generate Nb-rich melts, such that high-temperature leucosomes, in addition to related A2-type granites, may represent significant Nb deposits.
WOS关键词NORTH CHINA CRATON ; ULTRAHIGH-TEMPERATURE METAMORPHISM ; ZIRCON U-PB ; HIGH-PRESSURE GRANULITES ; HIGH-GRADE METAMORPHISM ; A-TYPE GRANITOIDS ; HIGHLAND COMPLEX ; SRI-LANKA ; SAPPHIRINE-BEARING ; TRACE-ELEMENTS
资助项目National Natural Science Foundation of China[41890832] ; National Natural Science Foundation of China[41902057] ; National Natural Science Foundation of China[41822202] ; National Natural Science Foundation of China[42172217] ; Program of China-Sri Lanka Joint Center for Water Technology Research and Demonstration by the Chinese Academy of Sciences (CAS) ; China-Sri Lanka Joint Center for Education and Research by the CAS
WOS研究方向Geochemistry & Geophysics ; Mineralogy
语种英语
WOS记录号WOS:000877187100004
出版者MINERALOGICAL SOC AMER
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Program of China-Sri Lanka Joint Center for Water Technology Research and Demonstration by the Chinese Academy of Sciences (CAS) ; Program of China-Sri Lanka Joint Center for Water Technology Research and Demonstration by the Chinese Academy of Sciences (CAS) ; Program of China-Sri Lanka Joint Center for Water Technology Research and Demonstration by the Chinese Academy of Sciences (CAS) ; Program of China-Sri Lanka Joint Center for Water Technology Research and Demonstration by the Chinese Academy of Sciences (CAS) ; China-Sri Lanka Joint Center for Education and Research by the CAS ; China-Sri Lanka Joint Center for Education and Research by the CAS ; China-Sri Lanka Joint Center for Education and Research by the CAS ; China-Sri Lanka Joint Center for Education and Research by the CAS ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Program of China-Sri Lanka Joint Center for Water Technology Research and Demonstration by the Chinese Academy of Sciences (CAS) ; Program of China-Sri Lanka Joint Center for Water Technology Research and Demonstration by the Chinese Academy of Sciences (CAS) ; Program of China-Sri Lanka Joint Center for Water Technology Research and Demonstration by the Chinese Academy of Sciences (CAS) ; Program of China-Sri Lanka Joint Center for Water Technology Research and Demonstration by the Chinese Academy of Sciences (CAS) ; China-Sri Lanka Joint Center for Education and Research by the CAS ; China-Sri Lanka Joint Center for Education and Research by the CAS ; China-Sri Lanka Joint Center for Education and Research by the CAS ; China-Sri Lanka Joint Center for Education and Research by the CAS ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Program of China-Sri Lanka Joint Center for Water Technology Research and Demonstration by the Chinese Academy of Sciences (CAS) ; Program of China-Sri Lanka Joint Center for Water Technology Research and Demonstration by the Chinese Academy of Sciences (CAS) ; Program of China-Sri Lanka Joint Center for Water Technology Research and Demonstration by the Chinese Academy of Sciences (CAS) ; Program of China-Sri Lanka Joint Center for Water Technology Research and Demonstration by the Chinese Academy of Sciences (CAS) ; China-Sri Lanka Joint Center for Education and Research by the CAS ; China-Sri Lanka Joint Center for Education and Research by the CAS ; China-Sri Lanka Joint Center for Education and Research by the CAS ; China-Sri Lanka Joint Center for Education and Research by the CAS ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Program of China-Sri Lanka Joint Center for Water Technology Research and Demonstration by the Chinese Academy of Sciences (CAS) ; Program of China-Sri Lanka Joint Center for Water Technology Research and Demonstration by the Chinese Academy of Sciences (CAS) ; Program of China-Sri Lanka Joint Center for Water Technology Research and Demonstration by the Chinese Academy of Sciences (CAS) ; Program of China-Sri Lanka Joint Center for Water Technology Research and Demonstration by the Chinese Academy of Sciences (CAS) ; China-Sri Lanka Joint Center for Education and Research by the CAS ; China-Sri Lanka Joint Center for Education and Research by the CAS ; China-Sri Lanka Joint Center for Education and Research by the CAS ; China-Sri Lanka Joint Center for Education and Research by the CAS
源URL[http://ir.iggcas.ac.cn/handle/132A11/107712]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Huang, Guangyu
作者单位1.Univ Oxford, Dept Earth Sci, Oxford OX1 3AN, England
2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
推荐引用方式
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Huang, Guangyu,Chen, Yi,Guo, Jinghui,et al. Nb and Ta intracrustal differentiation during granulite-facies metamorphism: Evidence from geochemical data of natural rocks and thermodynamic modeling[J]. AMERICAN MINERALOGIST,2022,107(11):2020-2033.
APA Huang, Guangyu,Chen, Yi,Guo, Jinghui,Palin, Richard,&Zhao, Lei.(2022).Nb and Ta intracrustal differentiation during granulite-facies metamorphism: Evidence from geochemical data of natural rocks and thermodynamic modeling.AMERICAN MINERALOGIST,107(11),2020-2033.
MLA Huang, Guangyu,et al."Nb and Ta intracrustal differentiation during granulite-facies metamorphism: Evidence from geochemical data of natural rocks and thermodynamic modeling".AMERICAN MINERALOGIST 107.11(2022):2020-2033.

入库方式: OAI收割

来源:地质与地球物理研究所

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