Low-Ca Pyroxene in Amoeboid Olivine Aggregates in Primitive Carbonaceous Chondrites

Physics

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Scientific paper

We report a discovery of low-Ca pyroxene in AOAs from CV, CR, CM, and
ungrouped carbonaceous chondrites Adelaide and Acfer 094 that formed by
reaction between 16O-rich forsterite (d17,18 ~ -40?), and SiO gas that
was depleted in 16O (delta-17,18 O ~ 0?).

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