Outside of that is a ring in
which pyroxene mixes with the standard crustal rocks of the lunar highlands.
Not exact matches
Earth's upper mantle,
which makes up much of the lithosphere, is a relatively simple mix, consisting primarily of two rock types, olivine and
pyroxene.
The scientists infer that late in the magma - ocean crystallization, iron - rich
pyroxene and ilmenite,
which formed late and at the crust - mantle boundary, might have begun to sink, and early - formed magnesium - rich olivine might have begun to rise.