Composition of the Lunar Maria

Computer Science

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Basalt: Mare, Mantle: Lunar, Mare Compositions, Maria: Lunar, Titanium

Scientific paper

We have developed analytical techniques to accurately determine the FeO and TiO2 contents from reflectance spectra, and applied these to a global data set (35-km spatial resolution) obtained by the Clementine mission. The data show that lunar mare basalts vary continuously in composition from very low-Ti to high-Ti basalts. Basalts with TiO2 contents in the range 2-4 wt.% are most abundant, though basalts with lower TiO2 are significant. Abundance decreases with increasing TiO2: only 5% of the mare surfaces contain >7.5 wt.% TiO2. This is consistent with the relative abundances of very-low to high-Ti cumulates produced in a magma ocean. Some maria have notably lower FeO (by at least 5 wt.%) than typical; these include Nectaris, Frigoris, and Orientale. These maria may be composed of basalts richer in Al2O3 than aluminous mare basalts in the sample collection.

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