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- W2039296333 abstract "High-P/T metamorphism of the Franciscan Complex represents evolving subduction-zone processes at depth. Varied peak P-T conditions (100–350°C and 3–10 kbar) promote differences in porosity, permeability, and rheology, potentially impacting fluid mobility and entrainment of seawater. Local-scale isotopic buffering of CaCO3 veins by exchange with adjacent host-rocks obscures assessment of fluid sources (most vein δ13CVPDB=−11.0 to −3.0‰, δ18OVSMOW=+12.0 to +18.5‰). Some veins with elevated δ18O (relative to rock-buffered values) may reflect up-dip flow of H2O released at greater depths. Differences in vein δ13C in adjacent coherent greywacke and shaley melange zones of lower-grade rocks may be due to preferential infiltration of melange zones by deeply derived CH4-bearing fluids or to vein formation over a range of T. Calculated fluid-δ18O for lower-T veins spans the range of fluids venting in active accretionary prisms and producing forearc serpentinite seamounts. Calcite cement in the Coastal Belt is absent in higher-grade rocks, suggesting that cement is lost to decarbonation reactions like those invoked to elevate fluid alkalinity in Marianas seamounts." @default.
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- W2039296333 date "2001-06-15" @default.
- W2039296333 modified "2023-09-27" @default.
- W2039296333 title "Paleohydrogeology at 5- to 50-kilometer depths of accretionary prisms: The Franciscan Complex, California" @default.
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- W2039296333 doi "https://doi.org/10.1029/2000gl008533" @default.
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