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- W1633150350 abstract "The composition of the parent magma for the Nakhla (martian) meteorite has been estimated from mineral-melt partitioning and from magmatic inclusions in olivine and in augite. These independent lines of evidence have converged on small range of likely compositions. Additional information is contained in the original extended abstract." @default.
- W1633150350 created "2016-06-24" @default.
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- W1633150350 date "2001-01-01" @default.
- W1633150350 modified "2023-09-23" @default.
- W1633150350 title "A Parent Magma for the Nakhla Martian Meteorite: Reconciliation of Estimates from 1-Bar Experiments, Magmatic Inclusions in Olivine, and Magmatic Inclusions in Augite" @default.
- W1633150350 hasPublicationYear "2001" @default.
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