Hydrogen Loss in Iron-bearing Mars Clays (or Palagonite) is Oxidation, not ``Dehydroxylation''

Details Hydrogen Loss in Iron-bearing Mars Clays (or Palagonite) is Oxidation, not ``Dehydroxylation'' Hydrogen Loss in Iron-bearing Mars Clays (or Palagonite) is Oxidation, not ``Dehydroxylation''

Mar 2002

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002lpi....33.1242b&link_type=abstract

33rd Annual Lunar and Planetary Science Conference, March 11-15, 2002, Houston, Texas, abstract no.1242

Computer Science

Scientific paper

The strongly oxidizing surface of Mars means that any ferrous clays have
lost hydrogen, forming oxy-clays that might be difficult to detect by
spectroscopy. This oxidation reaction has misleadingly been labelled
"dehydroxylation", which refers to thermal decomposition.

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