Abati Gómez, JacoboCastro Dorado, AntonioGómez Frutos, DanielGutiérrez Alonso, GabrielStockli, Daniel F.2026-03-042026-03-042025-10-23Morales, J., Gerding, J., Compaña, J. M., Astilleros García-Monge, J. M., Fernández-Díaz, L., & Gómez Barreiro, J. (2026). The growth of CaCO3 polymorphs in the presence of As(v): Stabilization of the vaterite phase. Environmental Science: Processes & Impacts, 28(2), 498-509. https://doi.org/10.1039/D5EM00364D0016-760610.1130/B38612.1https://hdl.handle.net/20.500.14352/133792The youngest granite suite of the Spanish Central System batholith (CSB) is classically interpreted as a post-collisional magmatic suite emplaced during the final stages of the Variscan orogeny. However, we report here for the first time the presence of discrete Andean-type plutons within the dominant post-collisional batholith. These plutons exhibit petrographic and geochemical signatures consistent with calc-alkaline series, including Ca-rich clinopyroxene and trace element trends that align with experimental cotectic arrays typical of active margin magmatism. MELTS modeling and phase-equilibrium constraints indicate that the parental magmas derived from a mantle-crust hybrid zone likely formed through localized recycling of oceanic-like mafic rocks during continental subduction. U-Pb zircon ages (312–306 Ma) confirm their temporal overlap with post-collisional granites. The low abundance of xenocrystic zircons (<5%) implies limited crustal assimilation, supporting a dominantly mantle-derived origin. We propose that back-arc basin closure and the subduction of hyperextended segments of Gondwana’s margin facilitated the transient involvement of oceanic components, generating conditions favorable for Andean-type magmatism within a nominally post-collisional context. This scenario challenges the conventional spatial and temporal dichotomy between Andean-type and post-collisional granite types and highlights the petrogenetic diversity inherent to late-orogenic magmatism. Our findings underscore the need to reassess current classification schemes for Variscan batholiths and advocate for integrated geochemical, petrographic, and geochronological approaches in unraveling complex source-to-pluton pathways.engAndean-type granites in a non-Andean post-collisional setting, Central System batholith, Spainjournal article1943-2674https://doi.org/10.1130/B38612.1https://pubs.geoscienceworld.org/gsa/gsabulletin/article/138/3-4/1547/662104/Andean-type-granites-in-a-non-Andean-postrestricted access552.32(460)Petrología2506.13 Petrología Ignea y Metamórfica