Weathering of Basaltic Rocks from the Gusev Plains up into the Columbia Hills from the Perspective of the MER Mössbauer Spectrometer

Details Weathering of Basaltic Rocks from the Gusev Plains up into the Columbia Hills from the Perspective of the MER Mössbauer Spectrometer Weathering of Basaltic Rocks from the Gusev Plains up into the Columbia Hills from the Perspective of the MER Mössbauer Spectrometer

Mar 2005

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2005lpi....36.2309s&link_type=abstract

36th Annual Lunar and Planetary Science Conference, March 14-18, 2005, in League City, Texas, abstract no.2309

Computer Science

1

Scientific paper

Mössbauer spectra of rocks at the foot of the Columbia Hills show a
decrease in olivine accompanied by an increase in the Fe-oxides
magnetite, hematite, and nanophase Fe3+-oxides, suggesting that chemical
weathering processes in the presence of water have altered these rocks
and outcrops.

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