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
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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 |
DOI | 10.1016/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. |
入库方式: OAI收割
来源:地质与地球物理研究所
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