Oxygen Isotopic Compositions of Calcium-Aluminum-rich Inclusions and Chondrules in the CB/CH-like Carbonaceous Chondrite Isheyevo

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Scientific paper

Oxygen isotopic compositions of the Isheyevo CAIs are similar to CAIs in
CH chondrites: 16O-rich CAIs are dominant whereas 16O-depleted CAIs are
rare. The latter most likely formed by remelting of the originally
16O-rich inclusions in an 16O-poor gaseous

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