Space scientists are keen to map the concentration of the titanium - dioxide -
rich mineral
ilmenite on the moon's surface, says Jim Garvin of NASA's Goddard Space Flight Center in Greenbelt, Maryland.
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.