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Moon-forming impactor as a source of Earth's basal mantle anomalies - Nature

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Moon-forming impactor as a source of Earth's basal mantle anomalies - Nature

Seismic images of Earth's interior have revealed two continent-sized anomalies with low seismic velocities, known as the large low-velocity provinces (LLVPs), in the lowermost mantle1. The LLVPs are often interpreted as intrinsically dense heterogeneities that are compositionally distinct from the surrounding mantle2. Here we show that LLVPs may represent buried relics of Theia mantle material (TMM) that was preserved in proto-Earth's mantle after the Moon-forming giant impact3.

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Moon-forming impactor as a source of Earth's basal mantle anomalies - Nature

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Moon-forming impactor as a source of Earth's basal mantle anomalies - Nature

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