Dual-process genesis for Valles Marineris basins and troughs on Mars

Mathematics – Logic

Scientific paper

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Mars Surface, Structural Basins, Planetary Crusts, Rocks, Planetary Structure, Geological Faults, Tectonics, Planetary Evolution, Satellite Imagery

Scientific paper

An improved sequence of formation for Valles Marineris depressions is proposed. It involves three key stages: (a) dike emplacement radial to Syria Planum during Late Noachian to Early Hesperian time; (b) subsidence of crustal rocks due to reduction of void space at depth during post-Early Hesperian time; and (c) regional normal faulting that overprints the ancestral basins and forms the structural troughs during Amazonian time.

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