A corundum-rich inclusion in the Murchison carbonaceous chondrite

Computer Science

Scientific paper

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Aluminum Oxides, Carbonaceous Chondrites, Inclusions, Ion Probes, Magnesium Isotopes, Meteoritic Composition, Abundance, Aluminum 27, Condensates, Hypervelocity Impact, Isotopic Enrichment, Refractory Materials, Thermodynamics, Data, Mass Spectrometry, Sem, Bb-5 Inclusion, Liquids, Origin, Melting, Samples, Terrestrial, Meteorite, Meteorites, Corundum, Hibonite, Carbonaceous Chondrites, Murchison Meteorite, Inclusions, Thermodynamics, Refractory Elements, Condensation, Electron Microprobe, Texture, Isotopes

Scientific paper

Although thermodynamic calculations predict corundum to be the first condensate from a cooling gas of solar composition, a corundum-hibonite inclusion, BB-5, has for the first time been found in the Murchison carbonaceous chondrite. Ion microprobe measurements of Mg isotopic compositions yield the result, unexpected in such an early condensate, that Mg-26 excesses are small despite large Al-27/Mg-24 ratios. The extreme temperature required to melt this inclusion makes a liquid origin unlikely, except by the hypervelocity impact of refractory bodies. Alternatively, B-5 is a direct gas-solid condensate, and its uniform Mg-26 enrichment must be a characteristic of the reservoir from which it condensed. Nebular heterogeneity in magnesium isotopic composition is the preferred explanation for the formation of such a reservoir.

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