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      An integrated view of the chemistry and mineralogy of martian soils

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          A Global View of Martian Surface Compositions from MGS-TES

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            Jarosite and hematite at Meridiani Planum from Opportunity's Mossbauer Spectrometer.

            Mossbauer spectra measured by the Opportunity rover revealed four mineralogical components in Meridiani Planum at Eagle crater: jarosite- and hematite-rich outcrop, hematite-rich soil, olivine-bearing basaltic soil, and a pyroxene-bearing basaltic rock (Bounce rock). Spherules, interpreted to be concretions, are hematite-rich and dispersed throughout the outcrop. Hematitic soils both within and outside Eagle crater are dominated by spherules and their fragments. Olivine-bearing basaltic soil is present throughout the region. Bounce rock is probably an impact erratic. Because jarosite is a hydroxide sulfate mineral, its presence at Meridiani Planum is mineralogical evidence for aqueous processes on Mars, probably under acid-sulfate conditions.
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              Detection of crystalline hematite mineralization on Mars by the Thermal Emission Spectrometer: Evidence for near-surface water

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                Author and article information

                Journal
                Nature
                Nature
                Springer Nature
                0028-0836
                1476-4687
                July 7 2005
                July 7 2005
                : 436
                : 7047
                : 49-54
                Article
                10.1038/nature03637
                16001059
                fdf16a14-4ec6-4df2-b9a2-a4d0c98ec710
                © 2005
                History

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