A Likely Formation Mechanism of the Hematite-rich Spherules in the Equatorial Region of Western Mars

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Scientific paper

We argue that the hematite-rich spherules were originally formed in
Valles Marineris and transported to Meridiani Planum accompanied with
accretion of finer volcanic materials, abrasion of basaltic fragments
and break down of the spherules during the wash-out flows.

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