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- W2732171282 endingPage "2375" @default.
- W2732171282 startingPage "2355" @default.
- W2732171282 abstract "The interplay between fluid mobility and deformation along subduction zone interfaces, and its influence on subduction C flux and other chemical cycling, can be evaluated through study of exposed paleo-subduction suites. Along traverses of three interface exposures in the Western Alps (Switzerland and Italy), lowering of carbonate δ18O values toward the fault surfaces is consistent with infiltration by H2O-rich fluid with δ18OVSMOW of +8.5 to +10.5‰ calculated using temperatures of 400–460 °C from Raman spectroscopy of carbonaceous matter. The lowering of δ18O occurs in rocks showing pervasive mylonitization and flattening parallel to the paleo-interface, and containing abundant deformed carbonate ± quartz veins, consistent with the enhancement of fluid infiltration by this deformation. These δ18O values could reflect mixtures of far-traveled fluids emanating from metabasaltic, meta-ultramafic, and metasedimentary sources at greater depths in the subducting slab (perhaps including hydrated mantle) and/or along the interface." @default.
- W2732171282 created "2017-07-14" @default.
- W2732171282 creator A5015773109 @default.
- W2732171282 creator A5042871219 @default.
- W2732171282 creator A5054708143 @default.
- W2732171282 date "2018-10-24" @default.
- W2732171282 modified "2023-09-30" @default.
- W2732171282 title "Deformation-enhanced fluid and mass transfer along Western and Central Alps paleo-subduction interfaces: Significance for carbon cycling models" @default.
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