Crustal Relaxation and Its Implications for the Martian Crustal Dichotomy

Physics

Scientific paper

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Scientific paper

Viscoelastic relaxation calculations show that the crustal dichotomy
would have relaxed in less than 1 Gy, given that the early crust was
relatively warm. We propose degree-1 mantle convection as a force to
maintain the dichotomy early on.

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