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.
Although the heat of the upper mantle might help the olivine or
pyroxene crystals within the rocks grow larger again, or «heal,» the two rock types are competing for space: Each is actually inhibited in its growth
by the other's presence.