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Geophysical evidence for an enriched molten silicate layer above Mars's core - Nature

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Geophysical evidence for an enriched molten silicate layer above Mars's core - Nature

The detection of deep reflected S waves on Mars inferred a core size of 1,830 ± 40 km (ref. 1), requiring light-element contents that are incompatible with experimental petrological constraints. This estimate assumes a compositionally homogeneous Martian mantle, at odds with recent measurements of anomalously slow propagating P waves diffracted along the core–mantle boundary2.

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Geophysical evidence for an enriched molten silicate layer above Mars's core - Nature

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Geophysical evidence for an enriched molten silicate layer above Mars's core - Nature

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