The Effect of Fe on OH- Content of Olivine: Implications for Extraction of H2O from the Martian Mantle

Details The Effect of Fe on OH- Content of Olivine: Implications for Extraction of H2O from the Martian Mantle The Effect of Fe on OH- Content of Olivine: Implications for Extraction of H2O from the Martian Mantle

Mar 2009

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2009lpi....40.1490w&link_type=abstract

40th Lunar and Planetary Science Conference, (Lunar and Planetary Science XL), held March 23-27, 2009 in The Woodlands, Texas, i

Physics

Scientific paper

Experimental determinations of the effect of Mg# on H2O storage capacity
in olivine + opx suggests that extraction of H2O from the martian mantle
is similar to that of a LREE. By analogy to K we infer that ~50% of
martian H2O remains in its mantle.

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