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Fluid flow in the subduction channel: Tremolite veins and associated blackwalls in antigoritite (Villa Clara serpentinite mélange, Cuba)
dc.contributor.author | Butjosa, Lidia | |
dc.contributor.author | Cambeses Torres, Aitor | |
dc.contributor.author | Proenza Fernández, Joaquín Antonio | |
dc.contributor.author | Blanco-Quintero, Idael Francisco | |
dc.contributor.author | Angostini, Samuele | |
dc.contributor.author | Iturralde, Manuel | |
dc.contributor.author | García Casco, Antonio | |
dc.date.accessioned | 2022-12-13T10:45:03Z | |
dc.date.available | 2022-12-13T10:45:03Z | |
dc.date.issued | 2022-12-01 | |
dc.identifier.citation | L. Butjosa et al. Fluid flow in the subduction channel: Tremolite veins and associated blackwalls in antigoritite (Villa Clara serpentinite mélange, Cuba). LITHOS 436–437 (2023) 106973 [https://doi.org/10.1016/j.lithos.2022.106973] | es_ES |
dc.identifier.uri | https://hdl.handle.net/10481/78420 | |
dc.description.abstract | Exotic blocks of massive antigorite-serpentinite (antigoritite) document a deep-seated subduction channel in the Villa Clara serpentinite-matrix m ́elange, central Cuba. The petrological and geochemical characteristics of antigoritite allow distinguishing two types of rock: i) antigoritite and ii) dolomite-bearing antigoritite. Both types are intimately related in field exposures and represent deep peridotite infiltrated by H2O-CO2 fluid mixtures that triggered antigoritization and local carbonation. Fluid infiltration continued after antigoritization forming a vein network as a potential response to hydrofracturing that precipitated tremolitite in the veins and triggered fluid- antigoritite reaction forming blackwalls. The mineralogical and chemical zoning in the blackwalls (Atg + Chl + Tr adjacent to antigoritite and Chl + Tr adjacent to the tremolitite vein) attest for multi-step metasomatic processes during fluid-rock interaction characterized by advection of infiltrating fluid towards the blackwall and, possibly, by diffusion out of the blackwall towards the fluid-filled vein. Tentative thermodynamic modeling of the blackwall domain Atg + Chl + Tr points vein network formation at 400–500 ◦C and 5–10 kbar during exhumation in the subduction channel, suggesting the infiltration of deep-seated pressurized fluid that triggered hydrofracturing. The chemical compositions of antigoritites, veins and blackwalls indicate a LILE- and LREE- enriched fluid evolved from the subducting plate, while Sr–Nd isotope systematics are compatible with an external fluid composed of a mixture of fluids evolved from sediments and, probably to a lesser extent, altered oceanic crust. | es_ES |
dc.description.sponsorship | Grupo RNM-302 | es_ES |
dc.description.sponsorship | MICINN PID2019- 105625RB-C21 (co-funded by Fondo Europeo de Desarrollo Regional, FEDER | es_ES |
dc.description.sponsorship | Junta de Andalucía P20_00550 | es_ES |
dc.description.sponsorship | Catalonian project SGR 2014- 1661 | es_ES |
dc.description.sponsorship | University of Granada | es_ES |
dc.description.sponsorship | Scholarship of Fundació Universitária Agustí Pedro i Pons | es_ES |
dc.description.sponsorship | Funding for open access charge: Universidad de Granada/CBUA | es_ES |
dc.description.sponsorship | PhD grant BES- 2013-063205 of the Spanish Ministry of Economy and Competitiveness | es_ES |
dc.language.iso | eng | es_ES |
dc.publisher | Elsevier | es_ES |
dc.rights | Attribution-NonCommercial-NoDerivatives 4.0 Internacional | * |
dc.rights.uri | http://creativecommons.org/licenses/by-nc-nd/4.0/ | * |
dc.subject | Antigoritite | es_ES |
dc.subject | Abyssal peridotite | es_ES |
dc.subject | Subduction | es_ES |
dc.subject | Fluid infiltration | es_ES |
dc.subject | Metasomatism | es_ES |
dc.subject | Mélange | es_ES |
dc.subject | Cuba | es_ES |
dc.subject | Caribbean | es_ES |
dc.title | Fluid flow in the subduction channel: Tremolite veins and associated blackwalls in antigoritite (Villa Clara serpentinite mélange, Cuba) | es_ES |
dc.type | journal article | es_ES |
dc.rights.accessRights | open access | es_ES |
dc.identifier.doi | https://doi.org/10.1016/j.lithos.2022.106973 | |
dc.type.hasVersion | VoR | es_ES |