Trace ferric ion in lunar and meteoritic titanaugites.
Evidence for presence of Fe(3+) in lunar rocks is furnished by heating them in air to 200-225 C for two hours. This causes a large decrease in the same charge transfer bands attributed to Fe(3+) that can be enhanced by heating the same rocks in air at 500 C. This is interpreted as evidence that the Fe(3+) was not in equilibrium in the melt but was produced by cosmic radiation subsequent to the rock formation. Possible tetrahedrally coordinated Fe(3+) is present in the meteoritic and lunar augites as suggested by comparison of their spectra to that of terrestrial augite high in Fe(3+). This would have been present in the original melt and is distinct from radiation produced Fe(3+) in the M-sites. The polarized absorption spectra of single crystal pigeonite and augite from rock 12021 before heating, and augite from 12018 after heating are compared to that of meteoritic titanaugite in the Angra dos Reis meteorite and terrestrial titanaugite from Maui, Hawaii. The absorption spectrum of meteoritic hypersthene (Tatahouine) is also included for comparison to the pigeonite.