Johannes Glodny, Michael Popov, Tom Raimondo, Samuel Angiboust, Patrick Monié, Antonio García-Casco, Aitor Cambeses, Angiboust, Samuel, Glodny, Johannes, Cambeses, Aitor, Raimondo, Tom, Monie, Patrick, Popov, Michael, Garcia-Casco, Antonio, Agence Nationale de la Recherche (France), Institut de Physique du Globe de Paris (IPGP), Institut national des sciences de l'Univers (INSU - CNRS)-IPG PARIS-Université de La Réunion (UR)-Centre National de la Recherche Scientifique (CNRS)-Université de Paris (UP), GeoForschungsZentrum - Helmholtz-Zentrum Potsdam (GFZ), University of South Australia [Adelaide], Géosciences Montpellier, Institut national des sciences de l'Univers (INSU - CNRS)-Université de Montpellier (UM)-Université des Antilles (UA)-Centre National de la Recherche Scientifique (CNRS), Institute of Geology and Geochemistry [Ekaterinburg] (IGG UB RAS), Ural Branch of Russian Academy of Sciences (UB RAS), Instituto Andaluz de Ciencias de la Tierra (IACT), Consejo Superior de Investigaciones Científicas [Madrid] (CSIC)-Universidad de Granada (UGR), Departamento de Mineralogia y Petrologia [Granada], and Universidad de Granada (UGR)
The physical and mechanical processes rooted in the hydrated, serpentinized mantle above subduction zones remain insufficiently explored despite fundamental implications for our understanding of rheology and fluid recycling along subduction interfaces. Through a field-based investigation, serpentinized peridotites and jadeitite samples from a fossil forearc mantle in the Polar Urals (Russia) are studied here to document fluid–rock interaction processes in the high-P field, as well as the long-term evolution of the base of the mantle wedge. Petrographic, geochemical and microstructural observations reveal a complex, protracted evolution of the jadeitite-forming fluid pathway throughout the gradual cooling of the forearc mantle and increasing serpentinization of the host. It is shown that the jadeitite lenses in the studied locality (a) derive for a large part from a trondhjemitic dyke earlier emplaced in a warm subduction environment, and (b) record the cooling of the subduction hangingwall under high-P conditions associated with increasing host serpentinization. In the studied locality, the majority of the jadeitites formed at relatively high temperatures (>600°C) by the influx of Na–Al-rich, slab-derived metamorphic fluids that were drained along the base of the mantle wedge, parallel to the subduction interface. Changes in bulk-rock geochemical signatures and in paragenetic sequences also constrain the compositional evolution of the fluid channelized along this drainage, with an increasing sedimentary component. The phlogopite-bearing walls of the dyke exhibit Rb–Sr and Ar–Ar ages ranging between c. 405 and c. 390 Ma, a range partly overlapping within uncertainty with the previously dated zircons from the jadeitite core (410–400 Ma; U–Pb). This study opens a unique window on the pristine structures formed above the plate interface by melting and fluid–rock interaction in the early subduction stages, as well as their evolution during secular cooling of the base of the mantle wedge., Agence Nationale de la Recherche, Grant/ Award Number: 16C538. Nicolas Rividi and Michel Fialin (CAMPARIS) are acknowledged for assistance with Electron Probe measurements and mapping. Michael Bostock is acknowledged for insightful discussions. This study was supported by the IdEx ANR-18-IDEX-0001 through a chair attributed to SA. Oleg, Firaz and Katia are acknowledged for assistance during the two field expeditions. The article was prepared when working on the state budget topic IGG UB RAS AAAA-A18-118052590032-6. Two reviewers are acknowledged for constructive comments. This is IPGP contribution #40XX.