中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Molybdenum systematics of subducted crust record reactive fluid flow from underlying slab serpentine dehydration

文献类型:期刊论文

作者Chen, Shuo3,4,5,6; Hin, Remco C.5; John, Timm2; Brooker, Richard5; Bryan, Ben5; Niu, Yaoling1,4,6; Elliott, Tim5
刊名NATURE COMMUNICATIONS
出版日期2019-10-21
卷号10页码:9
ISSN号2041-1723
DOI10.1038/s41467-019-12696-3
通讯作者Chen, Shuo(shuochen@qdio.ac.cn)
英文摘要Fluids liberated from subducting slabs are critical in global geochemical cycles. We investigate the behaviour of Mo during slab dehydration using two suites of exhumed fragments of subducted, oceanic lithosphere. Our samples display a positive correlation of delta Mo-98/95(NIST) (3134) with Mo/Ce, from compositions close to typical mantle (-0.2 parts per thousand and 0.03, respectively) to very low values of both delta Mo-98/95(NIST) (3134) ( -1 parts per thousand) and Mo/Ce (0.002). Together with new, experimental data, we show that molybdenum isotopic fractionation is driven by preference of heavier Mo isotopes for a fluid phase over rutile, the dominant mineral host of Mo in eclogites. Moreover, the strongly perturbed delta Mo-98/95(NIST) (3134) and Mo/Ce of our samples requires that they experienced a large flux of oxidised fluid. This is consistent with chan-nelised, reactive fluid flow through the subducted crust, following dehydration of the underlying, serpentinised slab mantle. The high delta Mo-98/95(NIST) (3134) of some arc lavas is the complement to this process.
资助项目Chinese NSF[41630968] ; Chinese NSF[41130314] ; Chinese NSF[41906050] ; Chinese NSF-Shandong[U1606401] ; UCAS Joint Ph.D. Training Program[UCAS[2015]37] ; [NE/M000419/1] ; [NE/L007428/1] ; [NE/J009024/1]
WOS研究方向Science & Technology - Other Topics
语种英语
WOS记录号WOS:000491223200001
出版者NATURE PUBLISHING GROUP
源URL[http://ir.qdio.ac.cn/handle/337002/163276]  
专题海洋研究所_海洋地质与环境重点实验室
通讯作者Chen, Shuo
作者单位1.Univ Durham, Dept Earth Sci, Durham DH1 3LE, England
2.Free Univ Berlin, Inst Geol Wissensch, Malteserstr 74-100, D-12249 Berlin, Germany
3.Chinese Acad Sci, Ctr Ocean Mega Sci, 7 Nanhai Rd, Qingdao 266071, Shandong, Peoples R China
4.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao 266061, Shandong, Peoples R China
5.Univ Bristol, Sch Earth Sci, Bristol Isotope Grp, Bristol BS8 1RJ, Avon, England
6.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Shandong, Peoples R China
推荐引用方式
GB/T 7714
Chen, Shuo,Hin, Remco C.,John, Timm,et al. Molybdenum systematics of subducted crust record reactive fluid flow from underlying slab serpentine dehydration[J]. NATURE COMMUNICATIONS,2019,10:9.
APA Chen, Shuo.,Hin, Remco C..,John, Timm.,Brooker, Richard.,Bryan, Ben.,...&Elliott, Tim.(2019).Molybdenum systematics of subducted crust record reactive fluid flow from underlying slab serpentine dehydration.NATURE COMMUNICATIONS,10,9.
MLA Chen, Shuo,et al."Molybdenum systematics of subducted crust record reactive fluid flow from underlying slab serpentine dehydration".NATURE COMMUNICATIONS 10(2019):9.

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来源:海洋研究所

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