Strategy for the In Situ Search of Evaporite and Carbonate Deposits in Gusev Crater Within the 2003 MER A Landing Ellipse

Physics

Scientific paper

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Scientific paper

Topographic profiles and MOC images suggest that the flat floor of Gusev
results from sediment deposition in the absence of strong sublacustrine
currents. This setting is favorable to preserve undisturbed sedimentary
sequences and identify carbonates and evaporites in the landing ellipse.

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