A Comprehensive Study of Pristine, Fine-grained, Spinel-rich Inclusions from the Leoville and Efremovka CV3 Chondrites, I: Petrology

Physics

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Scientific paper

Fine-grained spinel-rich CAI from Efremovka and Leoville lack the
overprint of Na and Fe metasomatism seen in Allende. They contain
spinel, pyroxene, anorthite, and melilite; most have a zoned structure
with spinel-rich cores, melilite-rich mantles.

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