Magnesium isotopic systematics of continental basalts from the North China craton: Implications for tracing subducted carbonate in the mantle
文献类型：期刊论文
| 作者 | Yang, Wei1,2,3; Teng, Fang-Zhen2,3; Zhang, Hong-Fu1; Li, Shu-Guang4,5 |
| 刊名 | CHEMICAL GEOLOGY
 |
| 出版日期 | 2012-10-18 |
| 卷号 | 328页码:185-194 |
| 关键词 | Magnesium isotopes Continental basalt Recycled carbonate The western Pacific oceanic subduction The North China craton |
| ISSN号 | 0009-2541 |
| DOI | 10.1016/j.chemgeo.2012.05.018 |
| 文献子类 | Article |
| 英文摘要 | To explore the possibility of tracing recycled carbonate by using Mg isotopes and to evaluate the effects of the western Pacific oceanic subduction on the upper mantle evolution of the North China craton, Mg isotopic compositions of the Mesozoic-Cenozoic basalts and basaltic andesites from the craton have been investigated. The samples studied here come from a broad area in the craton with variable ages of 125-6 Ma, and can be divided into two groups based on geochemical features: the >120 Ma Yixian basalts and basaltic andesites, and the <110 Ma Fuxin and Taihang basalts. Our results indicate that these two groups have distinct Mg isotopic compositions. The >120 Ma Yixian basalts and basaltic andesites, with low Ce/Pb, Nb/U ratios and lower-crust like Sr-Nd-Pb isotopic compositions, have a mantle-like Mg isotopic composition, with delta Mg-26 values ranging from -0.31 parts per thousand to -0.25 parts per thousand and an average of -0.27 +/- 0.05 parts per thousand (2SD, n = 5). This suggests that continental crust contamination may strongly modify their Ce/Pb, Nb/U ratios and Sr-Nd-Pb isotopic compositions but do not influence their Mg isotopic compositions. By contrast, the <110 Ma basalts from Fuxin and Taihang exhibit lower delta Mg-26 values of -0.60 parts per thousand. to -0.42 parts per thousand., with an average of -0.46 +/- 0.10 parts per thousand. (2SD). Since these basalts still preserve mantle-like Sr-Nd-Pb isotopic compositions and Ce/Pb, Nb/U ratios and have high U/Pb and Th/Pb ratios similar to those of basalts, the light Mg isotopic composition is most likely derived from interaction of their mantle source with isotopically light recycled carbonate melt. Since the Tethys and Mongolia oceanic subductions from south and north toward the North China craton were terminated in the Triassic and light Mg isotopic signature in basalts did not appear before 120 Ma. the subducted Pacific oceanic crust could be the major source of the recycled carbonate. Therefore, this study not only presents an example to trace recycled carbonate using Mg isotopes but also confirms the important role of the western Pacific oceanic subduction in generating the <110 Ma basalts in the North China craton. (C) 2012 Elsevier B.V. All rights reserved. |
| WOS关键词 | SUBCONTINENTAL LITHOSPHERIC MANTLE ; MESOZOIC MAFIC MAGMATISM ; OCEAN ISLAND BASALTS ; EASTERN CHINA ; CENOZOIC BASALTS ; THERMAL-DIFFUSION ; SHANDONG PROVINCE ; HANNUOBA BASALTS ; MARINE-SEDIMENTS ; SILICATE MELTS |
| WOS研究方向 | Geochemistry & Geophysics |
| 语种 | 英语 |
| WOS记录号 | WOS:000310124900011 |
| 出版者 | ELSEVIER SCIENCE BV |
| 资助机构 | National Science Foundation of China(41173012 ; National Science Foundation of China(41173012 ; National Science Foundation(EAR-0838227 ; National Science Foundation(EAR-0838227 ; Arkansas Space Grant Consortium(SW19002) ; Arkansas Space Grant Consortium(SW19002) ; 90714008 ; 90714008 ; EAR-1056713) ; EAR-1056713) ; 91014007 ; 91014007 ; 40921002 ; 40921002 ; 40803011) ; 40803011) ; National Science Foundation of China(41173012 ; National Science Foundation of China(41173012 ; National Science Foundation(EAR-0838227 ; National Science Foundation(EAR-0838227 ; Arkansas Space Grant Consortium(SW19002) ; Arkansas Space Grant Consortium(SW19002) ; 90714008 ; 90714008 ; EAR-1056713) ; EAR-1056713) ; 91014007 ; 91014007 ; 40921002 ; 40921002 ; 40803011) ; 40803011) ; National Science Foundation of China(41173012 ; National Science Foundation of China(41173012 ; National Science Foundation(EAR-0838227 ; National Science Foundation(EAR-0838227 ; Arkansas Space Grant Consortium(SW19002) ; Arkansas Space Grant Consortium(SW19002) ; 90714008 ; 90714008 ; EAR-1056713) ; EAR-1056713) ; 91014007 ; 91014007 ; 40921002 ; 40921002 ; 40803011) ; 40803011) ; National Science Foundation of China(41173012 ; National Science Foundation of China(41173012 ; National Science Foundation(EAR-0838227 ; National Science Foundation(EAR-0838227 ; Arkansas Space Grant Consortium(SW19002) ; Arkansas Space Grant Consortium(SW19002) ; 90714008 ; 90714008 ; EAR-1056713) ; EAR-1056713) ; 91014007 ; 91014007 ; 40921002 ; 40921002 ; 40803011) ; 40803011) |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/84516]  |
| 专题 | 中国科学院地质与地球物理研究所 |
| 通讯作者 | Yang, Wei |
| 作者单位 | 1.Chinese Acad Sci, State Key Lab Lithospher Evolut, Inst Geol & Geophys, Beijing 10029, Peoples R China 2.Univ Arkansas, Isotope Lab, Dept Geosci, Fayetteville, AR 72701 USA 3.Univ Arkansas, Arkansas Ctr Space & Planetary Sci, Fayetteville, AR 72701 USA 4.Univ Sci & Technol China, Sch Earth & Space Sci, CAS Key Lab Crust Mantle Mat & Environm, Hefei 230026, Peoples R China 5.China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Beijing 100083, Peoples R China |
| 推荐引用方式 GB/T 7714 | Yang, Wei,Teng, Fang-Zhen,Zhang, Hong-Fu,et al. Magnesium isotopic systematics of continental basalts from the North China craton: Implications for tracing subducted carbonate in the mantle[J]. CHEMICAL GEOLOGY,2012,328:185-194. |
| APA | Yang, Wei,Teng, Fang-Zhen,Zhang, Hong-Fu,&Li, Shu-Guang.(2012).Magnesium isotopic systematics of continental basalts from the North China craton: Implications for tracing subducted carbonate in the mantle.CHEMICAL GEOLOGY,328,185-194. |
| MLA | Yang, Wei,et al."Magnesium isotopic systematics of continental basalts from the North China craton: Implications for tracing subducted carbonate in the mantle".CHEMICAL GEOLOGY 328(2012):185-194. |
入库方式： OAI收割
来源：地质与地球物理研究所
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