Genesis of Augite-bearing Ureilites; Evidence from LA-ICP-MS Analyses of Pyroxenes and Olivine

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Scientific paper

Ureilites are restites from partial melting of a chondritic precursor,
but some augite-bearing ureilites may be partially cumulate. To test
this hypothesis, we examined compositions of silicate minerals in select
augite-bearing ureilites with differing mg#.

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