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- W2531243551 abstract "Abstract Scapolite in granulite facies terranes provides a reservoir for volatile components such as sulphur and carbon in rocks that are otherwise considered ‘dry’. Formed at lower crustal conditions, the high‐S end‐member of scapolite, silvialite, is a major host of sulphur in granulites. Compositional and textural changes involving scapolite reveal that S‐rich scapolite becomes unstable during hydration and deformation at amphibolite facies conditions. Either scapolite changes composition, whereby SO 4 2− is exchanged for CO 3 2− or Cl − in its structure, or scapolite is replaced by amphibole and/or epidote. Sulphur that is released from silvialite is deposited as sulphides within the original silvialite grain boundaries and can remain relatively immobile in undeformed anorthosites. However, increased sulphide mobility is evident in areas of increased deformation and hydration. Reactions involving S‐bearing scapolite not only have important implications for sulphide deposition and the S‐cycle, but may also influence conductivity variation in the lower crust." @default.
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- W2531243551 date "2016-10-24" @default.
- W2531243551 modified "2023-09-27" @default.
- W2531243551 title "Sulphide formation from granulite-facies S-rich scapolite breakdown" @default.
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- W2531243551 doi "https://doi.org/10.1111/ter.12242" @default.
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