Heterogeneous O Isotopic Distributions in Melilite and Anorthite in a CAI from the Dar Al Gani 521 Meteorite (CV3)

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Scientific paper

Anorthite and melilite in a CAI in Dar al Gani 521 meteorite show two
distinct O isotopic compositions: 16O-rich and 16O-poor. Both groups of
anorthite grains show canonical 26Al/27Al initial ratios, suggesting a
very early reheating event.

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