Serpentinite-derived slab fluids control the oxidation state of the subarc mantle
文献类型：期刊论文
| 作者 | Zhang, Yuxiang1,2,3 ; Gazel, Esteban4; Gaetani, Glenn A.5; Klein, Frieder6
|
| 刊名 | SCIENCE ADVANCES
 |
| 出版日期 | 2021-11-01 |
| 卷号 | 7期号:48页码:7 |
| ISSN号 | 2375-2548 |
| DOI | 10.1126/sciadv.abj2515 |
| 通讯作者 | Zhang, Yuxiang(zhangyuxiang13@mails.ucas.ac.cn) ; Gazel, Esteban(egazel@cornell.edu) |
| 英文摘要 | Recent geochemical evidence confirms the oxidized nature of arc magmas, but the underlying processes that regulate the redox state of the subarc mantle remain yet to be determined. We established a link between deep subduction-related fluids derived from dehydration of serpentinite +/- altered oceanic crust (AOC) using B isotopes and B/Nb as fluid proxies, and the oxidized nature of arc magmas as indicated by Cu enrichment during magma evolution and V/Yb. Our results suggest that arc magmas derived from source regions influenced by a greater serpentinite (+/- AOC) fluid component record higher oxygen fugacity. The incorporation of this component into the subarc mantle is controlled by the subduction system's thermodynamic conditions and geometry. Our results suggest that the redox state of the subarc mantle is not homogeneous globally: Primitive arc magmas associated with flat, warm subduction are less oxidized overall than those generated in steep, cold subduction zones. |
| 资助项目 | National Science Foundation of China[91958213] ; Chinese Academy of Sciences[XDB42020402] ; Shandong Provincial Natural Science Foundation, China[ZR2020QD068] ; U.S. National Science Foundation[NSF EAR 1826673] ; U.S. National Science Foundation[OCE 1756349] |
| WOS研究方向 | Science & Technology - Other Topics |
| 语种 | 英语 |
| 出版者 | AMER ASSOC ADVANCEMENT SCIENCE |
| WOS记录号 | WOS:000722925100010 |
| 源URL | [http://ir.qdio.ac.cn/handle/337002/177269]  |
| 专题 | 海洋研究所_海洋地质与环境重点实验室 |
| 通讯作者 | Zhang, Yuxiang; Gazel, Esteban |
| 作者单位 | 1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao, Shandong, Peoples R China 2.Qingdao Pilot Natl Lab Marine Sci & Technol, Lab Marine Mineral Resources, Qingdao, Shandong, Peoples R China 3.Chinese Acad Sci, Ctr Ocean Megasci, Qingdao, Shandong, Peoples R China 4.Cornell Univ, Dept Earth & Atmospher Sci, Ithaca, NY 14850 USA 5.Woods Hole Oceanog Inst, Dept Geol & Geophys, Woods Hole, MA 02543 USA 6.Woods Hole Oceanog Inst, Dept Marine Chem & Geochem, Woods Hole, MA 02543 USA |
| 推荐引用方式 GB/T 7714 | Zhang, Yuxiang,Gazel, Esteban,Gaetani, Glenn A.,et al. Serpentinite-derived slab fluids control the oxidation state of the subarc mantle[J]. SCIENCE ADVANCES,2021,7(48):7. |
| APA | Zhang, Yuxiang,Gazel, Esteban,Gaetani, Glenn A.,&Klein, Frieder.(2021).Serpentinite-derived slab fluids control the oxidation state of the subarc mantle.SCIENCE ADVANCES,7(48),7. |
| MLA | Zhang, Yuxiang,et al."Serpentinite-derived slab fluids control the oxidation state of the subarc mantle".SCIENCE ADVANCES 7.48(2021):7. |
入库方式： OAI收割
来源：海洋研究所
浏览0
下载0
收藏0
其他版本
除非特别说明，本系统中所有内容都受版权保护，并保留所有权利。