Mid-Latitude Amazonian Glaciation on Mars: Controls on Accumulation and Glacial Flow Patterns

Physics

Scientific paper

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Scientific paper

A model of flow into a crater from episodic layering events driven by
obliquity demonstrates that even at Amazonian temperatures, concentric
crater fill can be formed in as little as 50 m.y., whereas flow from a
single persistent layer takes 450 m.y.

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