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Vestiges of a lunar ilmenite layer following mantle overturn revealed by gravity data - Nature Geoscience

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Vestiges of a lunar ilmenite layer following mantle overturn revealed by gravity data - Nature Geoscience

The lunar crust and mantle formed through the crystallization of a magma ocean, culminating in a solid cumulate mantle with a layer of dense ilmenite-bearing cumulates rich in incompatible elements forming above less dense cumulates. This gravitationally unstable configuration probably resulted in a global mantle overturn, with ilmenite-bearing cumulates sinking into the interior.

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Vestiges of a lunar ilmenite layer following mantle overturn revealed by gravity data - Nature Geoscience

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Vestiges of a lunar ilmenite layer following mantle overturn revealed by gravity data - Nature Geoscience

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