Viscous Creep Relaxation of Impact Craters Within the Martian Polar Layered Deposits

Physics

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Scientific paper

Our finite-element simulations of impact craters within the Martian
Polar Layered Deposits (PLD) indicate that viscous creep relaxation of
dusty PLD ice is the resurfacing mechanism most consistent with both the
size distribution and ubiquitous shallowness of PLD craters.

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