Earth accreted homogeneously and exclusively from inner solar system material whose average composition was unlike any chondrite, as shown by its position on the NC isotopic array in all ten nucleosynthetic anomalies examined.
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Homogeneous accretion of the Earth in the inner Solar System
Earth accreted homogeneously and exclusively from inner solar system material whose average composition was unlike any chondrite, as shown by its position on the NC isotopic array in all ten nucleosynthetic anomalies examined.