Lunar Magma Ocean Crust: Implications of FeO Contents in Plagioclase

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Scientific paper

The FeO and MgO compositions of the highland plagioclase, particularly
that in the FANs, do not represent those from the original LMO. The
re-equilibrated values are due to slow cooling of the proto-crust,
similar to anorthosites on Earth (Phinney, 1991).

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