Mare basalt petrogenesis

Computer Science

Scientific paper

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Basalt, Chemical Composition, Lunar Evolution, Lunar Maria, Lunar Rocks, Vacuum Melting, Crystallization, Lunar Mantle, Petrography, Selenology, Titanium, Vacuum Effects

Scientific paper

Melting experiments in vacuum at Fe-saturation for high-Ti lunar basalt compositions 70215 and 15318 Red Glass, and low-Ti basalt composition 15555-15016, have defined equilibrium crystallization sequences and the liquid lines of descent, and show that much of the chemical variety in the samples is due to near-surface fractionation processes. The various groups within the high-Ti suite, however, cannot be interrelated by such processes, nor can the high-Ti suite be a near-surface derivative of a low-Ti parent magma.

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