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- W2287890 abstract "Forsterite-bearing type B refractory inclusions (FoBs) are unusual because a disproportionate fraction of the known examples possess mass-dependent isotopic fractionation in magnesium, silicon, and oxygen [1-3] that correlates with petrological evidence for melt distillation. All have textures broadly consistent with solidification of a silicate melt, but their outer aluminium-rich mantles have mineral assemblages that are petrologically incompatible with their interiors [2-4]. Many have an extreme patchiness of mineral distribution (“islands”) that cannot be explained by melt solidification alone. We previously [4] interpreted these textures as evidence that melt evaporation and hybridization both played a role in the formation of these objects. Here we give new bulk compositional data that relate directly to the nature of the hybridization process." @default.
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- W2287890 date "2007-08-01" @default.
- W2287890 modified "2023-09-23" @default.
- W2287890 title "Forsterite-bearing Type B CAIs: Bulk Composition Evidence for a Hybrid Origin" @default.
- W2287890 hasPublicationYear "2007" @default.
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