Oxygen Isotopic Composition of Individual Chondrules in an Enstatite Chondrite Yamato 791810

Physics

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Scientific paper

Oxygen isotopes were measured for chondrules from an EH4-chondrite to
elucidate the origin of noble-gas-rich chondrules. A porphyritic
pyroxene chondrule shows 16O excess and internal variation, suggesting
that the precursor contains 16O-rich grains.

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