中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Isotopic composition of Mg and Fe in garnet peridotites from the Kaapvaal and Siberian cratons

文献类型:期刊论文

作者An, Yajun1; Huang, Jin-Xiang2,3; Griffin, W. L.2,3; Liu, Chuanzhou4; Huang, Fang1
刊名GEOCHIMICA ET COSMOCHIMICA ACTA
出版日期2017-03-01
卷号200页码:167-185
关键词Garnet Peridotites Magnesium Isotopes Iron Isotopes Lithospheric Mantle Metasomatism
ISSN号0016-7037
DOI10.1016/j.gca.2016.11.041
文献子类Article
英文摘要We present Mg and Fe isotopic data for whole rocks and separated minerals (olivine, clinopyroxene, orthopyroxene, garnet, and phlogopite) of garnet peridotites that equilibrated at depths of 134-186 km beneath the Kaapvaal and Siberian cratons. There is no clear difference in delta(26) Mg and delta(56) Fe of garnet peridotites from these two cratons. delta(26) Mg of whole rocks varies from -0.243% to - 0.204% with an average of -0.225 +/- 0.037% (2 sigma, n = 19), and delta(56) Fe from -0.038% to 0.060% with an average of -0.003 +/- 0.068% (2 sigma, n = 19). Both values are indistinguishable from the fertile upper mantle, indicating that there is no significant Mg-Fe isotopic difference between the shallow and deep upper mantle. The garnet peridotites from ancient cratons show d 26 Mg similar to komatiites and basalts, further suggesting that there is no obvious Mg isotopic fractionation during different degrees of partial melting of deep mantle peridotites and komatiite formation.
WOS关键词NORTH CHINA CRATON ; LA-ICP-MS ; LITHOSPHERIC MANTLE BENEATH ; UDACHNAYA-EAST KIMBERLITE ; TRACE-ELEMENT EVIDENCE ; OXYGEN FUGACITY ; RE-OS ; EXPERIMENTAL CALIBRATION ; ORTHO-PYROXENE ; SOUTH-AFRICA
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000396792700010
出版者PERGAMON-ELSEVIER SCIENCE LTD
资助机构National Science Foundation of China(41603004 ; 111 Project ; Anhui Provincial Natural Science Foundation(1608085QD74) ; Fundamental Research Funds for the Central Universities ; 41325011 ; 41173031 ; 40873009 ; 41273045) ; National Science Foundation of China(41603004 ; 111 Project ; Anhui Provincial Natural Science Foundation(1608085QD74) ; Fundamental Research Funds for the Central Universities ; 41325011 ; 41173031 ; 40873009 ; 41273045) ; National Science Foundation of China(41603004 ; 111 Project ; Anhui Provincial Natural Science Foundation(1608085QD74) ; Fundamental Research Funds for the Central Universities ; 41325011 ; 41173031 ; 40873009 ; 41273045) ; National Science Foundation of China(41603004 ; 111 Project ; Anhui Provincial Natural Science Foundation(1608085QD74) ; Fundamental Research Funds for the Central Universities ; 41325011 ; 41173031 ; 40873009 ; 41273045)
源URL[http://ir.iggcas.ac.cn/handle/132A11/52994]  
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, Fang
作者单位1.Univ Sci & Technol China, Sch Earth & Space Sci, CAS Key Lab Crust Mantle Mat & Environm, Hefei 230026, Anhui, Peoples R China
2.Macquarie Univ, Australian Res Council Ctr Excellence Core Crust, Sydney, NSW 2109, Australia
3.Macquarie Univ, GEMOC, Sydney, NSW 2109, Australia
4.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
An, Yajun,Huang, Jin-Xiang,Griffin, W. L.,et al. Isotopic composition of Mg and Fe in garnet peridotites from the Kaapvaal and Siberian cratons[J]. GEOCHIMICA ET COSMOCHIMICA ACTA,2017,200:167-185.
APA An, Yajun,Huang, Jin-Xiang,Griffin, W. L.,Liu, Chuanzhou,&Huang, Fang.(2017).Isotopic composition of Mg and Fe in garnet peridotites from the Kaapvaal and Siberian cratons.GEOCHIMICA ET COSMOCHIMICA ACTA,200,167-185.
MLA An, Yajun,et al."Isotopic composition of Mg and Fe in garnet peridotites from the Kaapvaal and Siberian cratons".GEOCHIMICA ET COSMOCHIMICA ACTA 200(2017):167-185.

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来源:地质与地球物理研究所

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