Fe3+/ΣFe Ratios in Pigeonite as a Function of fO2: A Preliminary Investigation

Details Fe3+/ΣFe Ratios in Pigeonite as a Function of fO2: A Preliminary Investigation Fe3+/ΣFe Ratios in Pigeonite as a Function of fO2: A Preliminary Investigation

Mar 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003lpi....34.1361m&link_type=abstract

34th Annual Lunar and Planetary Science Conference, March 17-21, 2003, League City, Texas, abstract no.1361

Physics

5

Scientific paper

We present an experimental investigation into the partitioning of
Fe3+/Fe2+ between pigeonite and a basaltic shergottite melt as a
function of fO2. Once calibrated, this could serve as a potential
oxybarometer for the martian meteorites.

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