Could sedimentary carbonates be recycled into the lower mantle? Constraints from Mg isotopic composition of Emeishan basalts | |
Tian, Heng-Ci1,2; Yang, Wei1; Li, Shu-Guang3; Ke, Shan3 | |
刊名 | LITHOS |
2017-11-01 | |
卷号 | 292页码:250-261 |
关键词 | Mg Isotope Low-ti And High-ti Basalts Mantle Plume Recycled Sedimentary Carbonate |
ISSN号 | 0024-4937 |
DOI | 10.1016/j.lithos.2017.09.007 |
文献子类 | Article |
英文摘要 | Whether or not sedimentary carbonates can be recycled into the lower mantle through subduction remains unclear. To further elucidate this issue, we investigate the Mg isotopic composition of Permian basalts from the Emeishan large igneous province (ELIP). Emeishan basalts can be divided into two major groups: the low-Ti and high-Ti basalts, which exhibit distinct major, trace element, and Sr-Nd-Pb isotopic compositions. However, they both possess mantle-like Mg isotopic compositions with delta Mg-26 values of -033 to -0.19%. and -0.35 to -0.19%0, respectively. Both the low-Ti and high-Ti basalts have experienced compositional evolution, e.g., fractional crystallization or crustal contamination, because their Mg-# (39.8-61.1) values are significantly lower than that of primary melt (similar to 72.0). However, their delta Mg-26 values do not vary with Mg-# indicating that the Mg isotopic compositions of the basalts were inherited from their mantle source. The low-Ti basalts are enriched in light rare earth elements with low epsilon(Nd)(t) values (mostly ranging from -10.5 to -8.8) and low Ce/Pb, high Ba/Th ratios, suggesting that they were derived from the lithospheric mantle that was metasomatized by slab-derived fluids. Their mantle-like Mg isotopic composition suggests that the metasomatism of slab derived fluids did not affect their Mg isotopic composition. This is consistent with most of the reported Arc basalts with mantle-like Mg isotopic compositions. On the other hand, the high-Ti basalts display an OIB-like trace element pattern and positive epsilon(Nd)(t) values (+ 02 similar to + 2.1), which were possibly derived from a mantle plume that originated from the lower mantle. Their mantle-like Mg isotopic composition indicates that sedimentary carbonates recycled into the lower mantle beneath the ELIP were limited (<2%). (C) 2017 Elsevier B.V. All rights reserved. |
WOS关键词 | LARGE IGNEOUS PROVINCE ; PLUME-LITHOSPHERE INTERACTION ; NORTH CHINA CRATON ; IONIZATION MASS-SPECTROMETRY ; CONTINENTAL FLOOD BASALTS ; PERMIAN-TRIASSIC BOUNDARY ; SW CHINA ; SOUTHWESTERN CHINA ; EASTERN CHINA ; GEOCHEMICAL CONSTRAINTS |
WOS研究方向 | Geochemistry & Geophysics ; Mineralogy |
语种 | 英语 |
出版者 | ELSEVIER SCIENCE BV |
WOS记录号 | WOS:000416185500016 |
资助机构 | National Science Foundation of China(41322022 ; National Science Foundation of China(41322022 ; 41230209 ; 41230209 ; 41221002) ; 41221002) ; National Science Foundation of China(41322022 ; National Science Foundation of China(41322022 ; 41230209 ; 41230209 ; 41221002) ; 41221002) ; National Science Foundation of China(41322022 ; National Science Foundation of China(41322022 ; 41230209 ; 41230209 ; 41221002) ; 41221002) ; National Science Foundation of China(41322022 ; National Science Foundation of China(41322022 ; 41230209 ; 41230209 ; 41221002) ; 41221002) |
内容类型 | 期刊论文 |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/82092] |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Yang, Wei; Li, Shu-Guang |
作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Earth & Planetary Phys, Beijing 100029, Peoples R China 2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 3.China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Beijing 100083, Peoples R China |
推荐引用方式 GB/T 7714 | Tian, Heng-Ci,Yang, Wei,Li, Shu-Guang,et al. Could sedimentary carbonates be recycled into the lower mantle? Constraints from Mg isotopic composition of Emeishan basalts[J]. LITHOS,2017,292:250-261. |
APA | Tian, Heng-Ci,Yang, Wei,Li, Shu-Guang,&Ke, Shan.(2017).Could sedimentary carbonates be recycled into the lower mantle? Constraints from Mg isotopic composition of Emeishan basalts.LITHOS,292,250-261. |
MLA | Tian, Heng-Ci,et al."Could sedimentary carbonates be recycled into the lower mantle? Constraints from Mg isotopic composition of Emeishan basalts".LITHOS 292(2017):250-261. |
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