中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Hf-Nd isotopic decoupling in continental mantle lithosphere beneath Northeast China: Effects of pervasive mantle metasomatism

文献类型:期刊论文

作者Yu, Song-Yue1,2; Xu, Yi-Gang1; Huang, Xiao-Long1; Ma, Jin-Long1; Ge, Wen-Chun3; Zhang, Hui-Huang4; Qin, Xiu-Feng1
刊名JOURNAL OF ASIAN EARTH SCIENCES
出版日期2009-08-26
卷号35期号:6页码:554-570
关键词Peridotite xenoliths Geochemistry Hf-Nd isotopic decoupling Chromatographic metasomatism Lithospheric mantle NE China
ISSN号1367-9120
DOI10.1016/j.jseaes.2009.04.005
文献子类Article
英文摘要Nd-Hf isotopic decoupling has frequently been observed in the continental and oceanic mantle, but its origin remains controversial. Here we present combined elemental and Sr-Nd-Hf isotopic study on peridotite xenoliths entrained in Cenozoic basalts from Shuangliao and Jiaohe in Northeast China, which provides insight into this issue. The data reveal a heterogeneous lithospheric mantle beneath Northeastern China, consisting of fertile (type I) to strongly refractory (type II) peridotites. Type I peridotites are largely shielded from late metasomatism, thus preserving information of depletion events. Nd model age suggests a Proterozoic lithospheric mantle beneath NE China. Type II peridotites are mostly refractory harz-burgites and show ubiquitous enrichment of incompatible elements. They are further divided into two sub-groups. Clinopyroxenes from type IIa samples have high and wide Lu/Hf (0.34-1.3) and very radiogenic Hf isotopic ratios (epsilon(Hf) = 44.4-63.8). Hf concentration is generally low (0.12-0.43 ppm) and plots along or slightly above the modeled partial melting depletion trend. In contrast, Nd content in type IIa clinopyroxenes is significantly higher than the modeled concentrations in residues at a given degree of melt depletion. The difference in enrichment of Hf and Nd translates to decoupling of Lu/Hf-Sm/Nd ratios and of Nd-Hf isotopes (epsilon(Nd) = -1.3 to 8.4). Clinopyroxenes from most of type fib peridotites have relatively low Lu/Hf ratios (0.04-0.24) and coupled Nd-Hf isotopes. Both Hf and Nd plot significantly above the depletion trend; their concentrations are governed by the equilibrium partitioning between percolating melt and peridotites. The distinct geochemical characteristics of type IIa and type IIb clinopyroxenes may have resulted from chromatographic percolation of small volumes of silicate melts, in which percolation fronts of incompatible elements are dependent on their relative incompatibilities. (C) 2009 Elsevier Ltd. All rights reserved.
WOS关键词SPINEL-PERIDOTITE XENOLITHS ; SMALL MELT FRACTIONS ; EASTERN CHINA ; TRACE-ELEMENT ; NE CHINA ; SUBCONTINENTAL LITHOSPHERE ; ABYSSAL PERIDOTITES ; REFRACTORY MANTLE ; HIGH-TEMPERATURE ; ORTHO-PYROXENE
WOS研究方向Geology
语种英语
WOS记录号WOS:000267813800006
出版者PERGAMON-ELSEVIER SCIENCE LTD
资助机构National Science Foundation of China(70914001 ; National Science Foundation of China(70914001 ; CAS/SAFEA International Partnership Program for Creative Research Teams ; CAS/SAFEA International Partnership Program for Creative Research Teams ; 40673038) ; 40673038) ; National Science Foundation of China(70914001 ; National Science Foundation of China(70914001 ; CAS/SAFEA International Partnership Program for Creative Research Teams ; CAS/SAFEA International Partnership Program for Creative Research Teams ; 40673038) ; 40673038) ; National Science Foundation of China(70914001 ; National Science Foundation of China(70914001 ; CAS/SAFEA International Partnership Program for Creative Research Teams ; CAS/SAFEA International Partnership Program for Creative Research Teams ; 40673038) ; 40673038) ; National Science Foundation of China(70914001 ; National Science Foundation of China(70914001 ; CAS/SAFEA International Partnership Program for Creative Research Teams ; CAS/SAFEA International Partnership Program for Creative Research Teams ; 40673038) ; 40673038)
源URL[http://ir.iggcas.ac.cn/handle/132A11/70984]  
专题中国科学院地质与地球物理研究所
通讯作者Xu, Yi-Gang
作者单位1.Chinese Acad Sci, Guangzhou Inst Geochem, Key Lab Isotope Geochronol & Geochem, Guangzhou 510640, Guangdong, Peoples R China
2.Chinese Acad Sci, Inst Geochem, State Key Lab Ore Deposit Geochem, Guiyang 550002, Peoples R China
3.Jilin Univ, Coll Earth Sci, Changchun 130061, Peoples R China
4.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Yu, Song-Yue,Xu, Yi-Gang,Huang, Xiao-Long,et al. Hf-Nd isotopic decoupling in continental mantle lithosphere beneath Northeast China: Effects of pervasive mantle metasomatism[J]. JOURNAL OF ASIAN EARTH SCIENCES,2009,35(6):554-570.
APA Yu, Song-Yue.,Xu, Yi-Gang.,Huang, Xiao-Long.,Ma, Jin-Long.,Ge, Wen-Chun.,...&Qin, Xiu-Feng.(2009).Hf-Nd isotopic decoupling in continental mantle lithosphere beneath Northeast China: Effects of pervasive mantle metasomatism.JOURNAL OF ASIAN EARTH SCIENCES,35(6),554-570.
MLA Yu, Song-Yue,et al."Hf-Nd isotopic decoupling in continental mantle lithosphere beneath Northeast China: Effects of pervasive mantle metasomatism".JOURNAL OF ASIAN EARTH SCIENCES 35.6(2009):554-570.

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来源:地质与地球物理研究所

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