Halogens and noble gases in serpentinites and secondary peridotites: Implications for seawater subduction and the origin of mantle neon
Abstract
Ophiolitic serpentinites and secondary peridotites formed by serpentinite dehydration were investigated to improve constraints on the fates of noble gases and halogens during subduction zone metamorphism. The work extends previous studies to encompass F and four stages of serpentinization and serpentinite dehydration including: (i) oceanic serpentinites preserving the features of seafloor serpentinization; (ii) subducted high grade (olivine...
Paper Details
Title
Halogens and noble gases in serpentinites and secondary peridotites: Implications for seawater subduction and the origin of mantle neon
Published Date
Aug 1, 2018
Volume
235
Pages
285 - 304
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