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dc.contributor.authorXiong, Jia-Wei
dc.contributor.authorMarchesi, Claudio 
dc.contributor.authorPadrón Navarta, José Alberto 
dc.contributor.authorMenzel, Manuel D.
dc.contributor.authorGarrido, Carlos J.
dc.date.accessioned2023-10-16T11:03:48Z
dc.date.available2023-10-16T11:03:48Z
dc.date.issued2023-08-18
dc.identifier.citationXiong, J.-W., Chen, Y.-X., Shen, J., Marchesi, C., Scambelluri, M., Qin, L.-P., et al. (2023). Chromium isotope behavior during serpentinite dehydration in oceanic subduction zones. Journal of Geophysical Research: Solid Earth, 128, e2023JB026601. [https://doi. org/10.1029/2023JB026601]es_ES
dc.identifier.urihttps://hdl.handle.net/10481/85025
dc.description.abstractFluids released through the dehydration of serpentinite can be rich in Cl −, which enables the significant mobility of Cr in subduction zones. However, the Cr isotope behavior accompanying the mobility of Cr during serpentinite dehydration is still poorly constrained. Here, we report high-precision Cr isotope data for a unique suite of serpentinites that represent metamorphic products at different depths in oceanic subduction zones. Low-grade serpentinites affected by significant Cr loss during serpentinization exhibit remarkably higher δ 53Cr, while samples with Cr contents >∼1,800 ppm typically preserve mantle-like δ 53Cr. Antigorite serpentinites have an average δ 53Cr value of −0.17‰ ± 0.19‰ (n = 12, 2SD), which is statistically lower than those of low-grade serpentinite (−0.05‰ ± 0.30‰, n = 80, 2SD) and higher-grade chlorite harzburgite (−0.10‰ ± 0.27‰, n = 22, 2SD). This suggests that resolvable Cr isotope fractionation occurs during serpentinite dehydration, which is explained by the variability of Cr isotope behavior in the presence of Cl-bearing fluids at different dehydration stages. No obvious Cr isotope fractionation was found during chlorite harzburgite dehydration, probably related to the limited Cr mobility in a Cl-poor fluid. Other processes, such as melt extraction, external fluid influx and retrograde metamorphism, have negligible effects on the Cr isotope systematics of meta-serpentinites. Fluids released by serpentinite dehydration may have a great effect on the Cr isotope heterogeneity of mantle wedge peridotites and arc magmas.es_ES
dc.description.sponsorshipNational Key Ramp;D Program of Chinaes_ES
dc.description.sponsorshipStrategic Priority Research Program (B) of CAS 2018YFA0702600es_ES
dc.description.sponsorshipNational Natural Science Foundation of China (NSFC) XDB41000000es_ES
dc.description.sponsorshipFundamental Research Funds for the Central Universities 42073029 41973004es_ES
dc.description.sponsorshipCNSAes_ES
dc.description.sponsorshipMICIN/AEI D020204es_ES
dc.description.sponsorshipFEDER program "Una manera de hacer Europa" PID2022-136471N-B-C21 C22 PID2019-111715GB-I00es_ES
dc.description.sponsorshipAEIes_ES
dc.description.sponsorshipFSE program "FSE invierte en tu futuro" RYC2018-024363-Ies_ES
dc.description.sponsorshipJunta de Andaluciaes_ES
dc.description.sponsorshipEuropean Union (EU) Postdoc_21_00791es_ES
dc.description.sponsorshipEuropean Social Fund (ESF)es_ES
dc.description.sponsorshipJunta de Andalucia RNM-131 RNM-374es_ES
dc.language.isoenges_ES
dc.publisherWileyes_ES
dc.rightsAtribución 4.0 Internacional*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/*
dc.titleChromium Isotope Behavior During Serpentinite Dehydration in Oceanic Subduction Zoneses_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.projectIDinfo:eu-repo/grantAgreement/EC/European Union/Postdoc_21_00791es_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
dc.identifier.doi10.1029/2023JB026601
dc.type.hasVersioninfo:eu-repo/semantics/publishedVersiones_ES


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