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The Transition from Phyllosilicate to Hydrated Sulfate Deposition as Evidenced from Mars Reconnaissance Orbiter CRISM and Opportunity Rover Observations in Meridiani Planum

R. E. Arvidson, Jeffrey G. Catalano

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Key concepts: Orbiter, Astrobiology, Mars Exploration Program, Deposition (geology), Geology, Remote sensing, Aerospace engineering, Engineering

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The Transition from Phyllosilicate to Hydrated Sulfate Deposition as Evidenced from Mars Reconnaissance Orbiter CRISM and Opportunity Rover Observations in Meridiani Planum — Research Paper | ScholarLens