Multiple veining in a paleo–accretionary wedge: The metamorphic rock record of prograde dehydration and transient high porefluid pressures along the subduction interface (Western Series, central Chile) Muñoz Montecinos, Jesús Cambeses Torres, Aitor García Casco, Antonio Thaïs Hyppolito is acknowledged for sharing her knowledge about local geology. Anne Verlaguet, Hugues Raimbourg, and James Connolly are also acknowledged for insightful discussions on fluid-rock metamorphic processes. Ralf Halama and two anonymous reviewers are warmly acknowledged for insightful comments. Mauricio Calderón, Francisco Fuentes, and the Earth Sciences department at Universidad Andrés Bello (Santiago, Chile) are thanked for their technical assistance. A.C. acknowledges the research grant provided by the Alexander von Humboldt Foundation for a post-doctoral fellowship at Ruhr-Universität Bochum. High pressure–low temperature metamorphic rocks from the late Paleozoic accretionary wedge exposed in central Chile (Pichilemu region) are characterized by a greenschist-blueschist lithological association with interbedded metasediments that reached peak burial conditions of ~400 °C and 0.8 GPa during late Carboniferous times. We herein combine new extensive field observations, structural measurements, and geochemical and petrological data on vein and matrix material from Pichilemu transitional greenschist-blueschist facies rocks. The studied veins were first filled by albite, followed by quartz and calcite as well as glaucophane and winchite. Field, structural, and microscopic zoning patterns show that these rocks underwent a protracted sequence of prograde vein-opening events, which have been largely transposed to the main foliation before and during underplating in the basal accretion site near 25–30 km depth. While some of the earliest albite-filled vein sets may have formed after prograde breakdown of sub–greenschist facies minerals (<250 °C), our thermodynamic modeling shows that relatively minor amounts of fluid are produced in the subducted pile by dehydration reactions between 250 and 400 °C along the estimated geothermal gradient. It also confirms that the formation of interlayered blueschist and greenschist layers in Pichilemu metavolcanics is a consequence of local bulk composition variations, and that greenschists are generally not formed due to selective exhumation-related retrogression of blueschists. The early vein sets are a consequence of prograde internal fluid production followed by sets of hydrofractures formed at near-peak burial that are interpreted as a record of external fluid influx. We postulate that such a fractured sequence represents a close analogue to the high-Vp/Vs regions documented by seismological studies within the base of the seismogenic zone in active subduction settings. 2020-06-23T11:44:37Z 2020-06-23T11:44:37Z 2020-03 info:eu-repo/semantics/article Muñoz-Montecinos, J., Angiboust, S., Cambeses, A., and García-Casco, A., 2020, Multiple veining in a paleo–accretionary wedge: The metamorphic rock record of prograde dehydration and transient high pore-fluid pressures along the subduction interface (Western Series, central Chile): Geosphere, v. 16, no. 3, p. 765–786, [https://doi.org/10.1130/GES02227.1.] http://hdl.handle.net/10481/62668 10.1130/GES02227.1 eng http://creativecommons.org/licenses/by-nc/3.0/es/ info:eu-repo/semantics/openAccess Atribución-NoComercial 3.0 España Geological Society of America