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- W2552367747 abstract "Geochemically diverse mid-ocean ridge basalts recovered from the Siqueiros Transform Fault, in the east Pacific Ocean, were sulfide-saturated at eruption, on the basis of the presence of immiscible sulfide globules and major and trace element variations of pillow-rim glasses. Previous workers have interpreted, from the chemistry of silicate melt inclusions in olivines which crystallised from liquids more primitive than the erupted basalts, that early Siqueiros liquids were sulfide-undersaturated (e.g., Saal et al. 2002). However, as the composition of these melt inclusions may not represent primary liquid compositions (as discussed by Danyushevsky et al. 2003) and inclusions of immiscible sulfides occur in the olivines, we interpret that at least some of these liquids were sulfide-saturated early in their fractionation history. The compositions of the immiscible sulfide inclusions in olivine are consistent with those from other MORB suites and estimates of sulfide liquid compositions from mantle rocks (e.g., Lorand 1988). Data from the erupted basalts and inclusions provides a well constrained natural dataset that has been combined with experimental data to produce a new sulfide saturation model (Bychkov et al. 2009) and can be used to test the results of this model." @default.
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- W2552367747 date "2010-01-01" @default.
- W2552367747 modified "2023-09-26" @default.
- W2552367747 title "The Siqueiros Transform Fault MORB; A Tale of Sulfur- Saturation" @default.
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