Oxygen Isotopic Compositions of Phenocrysts in Chondrules from the Primitive Carbonaceous Chondrite Acfer 094

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Scientific paper

We measured O isotopic compositions of 29 chondrules from Acfer 094. We
found 16O-poor relict olivine from 3 chondrules, suggesting that their
precursors formed in a 16O-poor environment and were processed in a
relatively 16O-rich environment.

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