The Opening of the Valles Marineris Canyons on Mars: Stress Focusing Along the Buried Dichotomy Boundary Beneath Tharsis

Physics

Scientific paper

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Scientific paper

The Valles Marineris canyons formed as a result of Tharsis loading over
the preexisting crustal dichotomy boundary, which generated a narrow
belt of strongly extensional stresses just south of the boundary at the
present-day location of the canyons.

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