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- W2810313210 abstract "Abstract The chemical compositions of the residues of the mantle melting that produces mid-ocean ridge basalt can be altered by fluid–rock interactions at spreading ridges and, possibly, during seawater penetration along bending-related faults in plates approaching trenches. This chemically modified rock, if subducted deeply and after long-term residence within the deep Earth, is a potential source of chemical heterogeneity in the mantle. Here, we demonstrate that peridotites from the Horoman massif preserve the chemical signatures of sub-seafloor hydrothermal (SSH) alteration at a mid-ocean ridge approximately one billion years ago. These rocks have evolved chemically subsequent to this SSH alteration; however, they retain the SSH-associated enrichments in fluid mobile elements and H 2 O despite their long-term residence within the mantle. Our results indicate that ancient SSH alteration resulting in the production of sulfide leads to Pb enrichment that could affect the present-day Pb isotopic evolution of the silicate earth. Evidence from the Horoman massif of the recycling of hydrous refractory domains into the mantle suggests that both the flux of H 2 O content into the mantle and the size of the mantle H 2 O reservoir are higher than have been estimated recently." @default.
- W2810313210 created "2018-07-10" @default.
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- W2810313210 date "2018-06-29" @default.
- W2810313210 modified "2023-10-12" @default.
- W2810313210 title "Circa 1 Ga sub-seafloor hydrothermal alteration imprinted on the Horoman peridotite massif" @default.
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- W2810313210 doi "https://doi.org/10.1038/s41598-018-28219-x" @default.
- W2810313210 hasPubMedCentralId "https://www.ncbi.nlm.nih.gov/pmc/articles/6026181" @default.
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