Mars - Fretted terrain as eroded ejecta from the Borealis mega-impact origin for the crustal dichotomy

Physics

Scientific paper

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Mars (Planet), Planetary Crusts, Erosion, Terrain Analysis

Scientific paper

The proximity of unconsolidated fretted terrain to the proposed basin
result of the megaimpact theory for the crustal dichotomy on Mars
implies the possibility this unconsolidated fretted terrain may be
eroded deposits of a large ejecta blanket emplaced by the Borealis
mega-impact origin for the crustal dichotomy.

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