Northwest Africa 1500: A Plagioclase-bearing Monomict Ureilite

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Scientific paper

NWA 1500 is an olivine-rich meteorite, with significant augite and
plagioclase. We interpret it to be a cumulate ureilite, formed from a
melt produced in a deep, oxidized source region. Its plagioclase
represents the "missing basaltic component" from the UPB.

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