Acid Alteration of Basalts, Andesites, and Anorthosites: Near-IR Spectra and Implications for Martian Soil Formation

Details Acid Alteration of Basalts, Andesites, and Anorthosites: Near-IR Spectra and Implications for Martian Soil Formation Acid Alteration of Basalts, Andesites, and Anorthosites: Near-IR Spectra and Implications for Martian Soil Formation

Mar 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011lpi....42.2415h&link_type=abstract

42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas. LPI Contribution No. 1608, p.2415

Physics

1

Scientific paper

Laboratory experiments indicate that acid alteration causes
pH-dependent, observable changes to the near-IR spectra of mafic
minerals, likely due to differences in solubility. Observations suggest
that this process may have occurred in martian soils.

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