Oxygen isotopes in chondrules and coarse-grained chondrule rims from the Allende meteorite

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Allende Meteorite, Chondrule, Meteoritic Composition, Oxygen Isotopes, Carbonaceous Chondrites, Enstatite, Minerals, Meteorites, Allende, Oxygen, Isotopes, Chondrules, Composition, Rims, Samples, Meteorite, Cv3 Chondrites, Stony Meteorites, Depletion, Matrix, Chemistry, Comparisons, Laboratory Studies, Lithophiles, Porphyretics, Alkali, Volatiles, Refractory Material

Scientific paper

The relationship between the porphyritic chondrules and coase-grained chondrule rims of the Allende CV chondrite are examined. The oxygen isotopic compositions of seven chondrule-rim pairs and a large rimless refractory chondrule from Allende are determined. The results suggest that, to account for the O-isotopic compositions of the CV chondrules and rims, three solid precursor components are required: a high-temperature, refractory-, alkali, and (O-16)-rich component; a low-temperature, FeO-rich, refractory, and (O-16)-poor component, and an additional component to explain the composition of BO chondrules.

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