Isolated olivines in the Yamato 82042 CM2 chondrite - The tracing of major condensation events in the solar nebula

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Carbonaceous Chondrites, Meteoritic Composition, Olivine, Annealing, Cosmochemistry, Petrography, Silicates, Meteorites, Antarctic Meteorites, Yamato Meteorites, Yamato 82042, Olivine, Cm2 Chondrites, Condensation, Solar Nebula, Samples, Meteorite, Formation, Laboratory Studies, Microprobe Methods, Photomicrographs, Crystals, Origin, Condensates, Vapor, Data

Scientific paper

It is shown that the abundances, distributions, and correlations among minor element contents of olivines in Y-82042 (C2) chondrite are compatible with an origin for the crystals as solid crystalline condensates from a vapor. The first olivines to condense from that vapor were rich in Ca and Al, contained about 0.25 wt pct FeO and apparently cocondensed with a Ca-Al-rich liquid; this liquid is represented by Ca-Al-rich glass inclusions in the Ca-rich olivines.

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