Impact Surge as the Simplest of the Proposed Hypotheses for the Origin of Sediments at the Opportunity Landing Site on Mars

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Scientific paper

The MER Athena Team interpretation that sediments at the Opportunity
Landing Site on Mars are altered eolian sands derived from a wet playa
is complex and has difficulties. Newly published data further support
sedimentation from an impact surge followed by normal martian
weathering.

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