Evidence for Past Kilometer-Scale Overturn(s) in Deformed, Layered Terrain Near the Deepest Point on Mars

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Scientific paper

In NW Hellas, wind has exhumed layered terrain showing ductile
deformation. A km-scale cellular pattern is identified, consistent with
thermal and/or compositional convection. ‘Frozen-in’
convection within an impact melt sheet is consistent with observations.

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