Oxygen Isotopic Composition of Fine-grained Ca-Al-rich Inclusions in the Reduced CV3 Chondrite Efremovka

Physics

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Scientific paper

O isotopes were measured in 4 fine-grained CAIs from Efremovka. One CAI
has 16O-rich melilite and an outer type A-like zone with
16O-poor melilite. Various degrees of isotopic exchange from
core to rim of the CAIs seem associated to re-heating.

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