Earthshine-induced global circulation in the lunar magma ocean transports anorthositic crystals from the nearside to the farside, where cooler temperatures enable rapid crystallization and thicker crust formation.
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Origin of the lunar farside highlands from Earthshine-induced global circulation in lunar magma ocean
Earthshine-induced global circulation in the lunar magma ocean transports anorthositic crystals from the nearside to the farside, where cooler temperatures enable rapid crystallization and thicker crust formation.