Li and O isotopes of mantle xenoliths from deep fault-related Cenozoic basalts in eastern China: The role of subducted components in the generation of the heterogeneous lithospheric mantle
文献类型：期刊论文
| 作者 | Chen, Qiong3; Zhou, Mei-Fu2; Xia, Xiao-Ping4; Liu, Ping-Ping1 |
| 刊名 | CHEMICAL GEOLOGY
 |
| 出版日期 | 2023-06-30 |
| 卷号 | 628页码:15 |
| 关键词 | Peridotite Lithium isotopes Oxygen isotopes Pacific Ocean South China |
| ISSN号 | 0009-2541 |
| DOI | 10.1016/j.chemgeo.2023.121471 |
| 英文摘要 | It has been known that the lithospheric mantle underneath eastern China is geochemically heterogeneous, with different isotopic compositions across the South China and North China blocks. The distribution of Cenozoic basalts (<23 Ma) with abundant mantle xenoliths in eastern China is mainly controlled by lithospheric-scale faults. In this paper, we report new Li and O isotopic data for these mantle xenoliths and demonstrate that the mantle was variably modified via the Pacific subduction. Most olivine and orthopyroxene grains from the peridotite xenoliths in the South China block display lower delta 18O values (4.43 to 5.77%0 and 4.77 to 5.55%0; respectively) than those of normal mantle, possibly reflecting impregnation of the slab melt of altered gabbroic precursors in the mantle transition zone (MTZ). The positive correlation between Li (1.40-6.54 ppm) and delta 7Li (-28.41 to 20.83%0) of olivine grains suggests that the SCLM was metasomatized by hydrated slab-derived, isotopically heavier Li melts penetrating the frontal mantle wedge. The decoupling of Li and O isotopic sys-tems implies that both hydrated mantle wedge and MTZ control the mass transportation and melt/fluid flow circulation beneath South China via the Pacific subduction. Comparatively, the higher delta 18O values (4.90-6.41%0) and negative correlations between Li (1.39-6.02 ppm) and delta 7Li (-23.55 to 22.54%0) in olivine grains from the North China block suggest a major contribution from the eclogitic slab that was metasomatized by the carbo-natitic agent. Our findings corroborate the wide storage of carbonated eclogites in the MTZ beneath North China. We highlight that the stagnant slab in the MTZ might have controlled the refertilization of the lithospheric mantle beneath North China. |
| WOS研究方向 | Geochemistry & Geophysics |
| 语种 | 英语 |
| WOS记录号 | WOS:000982965800001 |
| 源URL | [http://ir.gig.ac.cn/handle/344008/74176]  |
| 专题 | 同位素地球化学国家重点实验室 |
| 通讯作者 | Zhou, Mei-Fu |
| 作者单位 | 1.Peking Univ, Sch Earth & Space Sci, Key Lab Orogen Belts & Crustal Evolut, Beijing 100871, Peoples R China 2.Chinese Acad Sci, Inst Geochem, State Key Lab Ore Deposit Geochem, Guiyang 550081, Peoples R China 3.Tongji Univ, Sch Ocean & Earth Sci, Shanghai 200092, Peoples R China 4.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Peoples R China |
| 推荐引用方式 GB/T 7714 | Chen, Qiong,Zhou, Mei-Fu,Xia, Xiao-Ping,et al. Li and O isotopes of mantle xenoliths from deep fault-related Cenozoic basalts in eastern China: The role of subducted components in the generation of the heterogeneous lithospheric mantle[J]. CHEMICAL GEOLOGY,2023,628:15. |
| APA | Chen, Qiong,Zhou, Mei-Fu,Xia, Xiao-Ping,&Liu, Ping-Ping.(2023).Li and O isotopes of mantle xenoliths from deep fault-related Cenozoic basalts in eastern China: The role of subducted components in the generation of the heterogeneous lithospheric mantle.CHEMICAL GEOLOGY,628,15. |
| MLA | Chen, Qiong,et al."Li and O isotopes of mantle xenoliths from deep fault-related Cenozoic basalts in eastern China: The role of subducted components in the generation of the heterogeneous lithospheric mantle".CHEMICAL GEOLOGY 628(2023):15. |
入库方式： OAI收割
来源：广州地球化学研究所
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