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.
Not exact matches
Humayun's team analyzed rock pieces
rich in
pyroxene and feldspar — minerals that would have been among the first to settle out of a cooling magma chamber.
Laboratory experiments show that under the conditions prevailing at these vents, ultramafic silicates — rocks
rich in iron or magnesium, such as olivine and
pyroxene — can react to produce hydrogen in a process commonly referred to as serpentinization.
The north - south variation in minerals indicates that the deep crust exposed in the southern Rheasilvia region is dominated by
pyroxene -
rich, diogenitic material while the equatorial region seems to retain the most ancient eucrite -
rich mineralogy.
The signatures of
pyroxene, an iron - and magnesium -
rich mineral, in these meteorites have been found to match those of rocks observed on Vesta's surface.