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- W2891903020 abstract "In the southeastern Oman Mountains the mantle section of the Samail ophiolite is unconformably capped by large units of Maastrichtian to Eocene limestones deposited in a shallow marine environment after ophiolite emplacement. In the vicinity of the town of Fins, a deep canyon carved by a stream has exposed mantle sections of the ophiolite. This section is composed of altered peridotites with high concentrations of calcium and small enrichments of silica compared to the Samail mantle protolith suggesting that the peridotites reacted with a hydrous fluid derived from interaction of seawater with the overlying sediments composed of limestones with minor amounts of chert. This is further affirmed by average δ13C (−0.25‰VPDB) δ18O (−5.53‰VPDB) and 87Sr/86Sr (0.70788) in the carbonate veins, consistent with values in the sediments. Clumped isotope thermometry on calcite veins in peridotite establish that they formed at 25–60 °C. Reaction path modeling of carbonate-quartz derived fluids with peridotite reproduces the observed mineral assemblage composed of carbonate and serpentine with similar Mg# and MgO/SiO2 at high water to rock ratios, with carbon, H2O and silica added to the rock by the reacting fluid." @default.
- W2891903020 created "2018-09-27" @default.
- W2891903020 creator A5032279664 @default.
- W2891903020 creator A5038547776 @default.
- W2891903020 date "2018-10-01" @default.
- W2891903020 modified "2023-09-25" @default.
- W2891903020 title "Fluid rock interactions on residual mantle peridotites overlain by shallow oceanic limestones: Insights from Wadi Fins, Sultanate of Oman" @default.
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- W2891903020 doi "https://doi.org/10.1016/j.chemgeo.2018.09.022" @default.
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