The Parent Magma of Ureilite Hughes 009 (Re-)Inferred from Melt Inclusions in Olivine: Implications for Petrogenesis of Augite-bearing Ureilites

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Scientific paper

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Scientific paper

The parent magma of augite-bearing ureilite Hughes 009 is re-derived
from melt inclusions in olivine. Methodological issues are discussed.
The new result has implications for petrogenesis of augite-bearing
ureilites.

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