Istopically Uniform, 16O-Depleted CAIs in Metal-Rich Carbonaceous Chondrites.

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Scientific paper

The metal-rich carbonaceous chondrites (CH, CB, and Isheyevo) contain a
population of igneous CAIs, which are isotopically uniform and
16O-depleted [D17O ~ -7‰] compared to CAIs from other chondrite
groups (D17O ~ -23.5‰), suggesting a unique origin.

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