Oxygen Fugacity of the Upper Mantle of Mars. Evidence from the Partitioning Behavior of Vanadium in Y980459 (Y98) and Other Olivine-Phyric Shergottites

Details Oxygen Fugacity of the Upper Mantle of Mars. Evidence from the Partitioning Behavior of Vanadium in Y980459 (Y98) and Other Olivine-Phyric Shergottites Oxygen Fugacity of the Upper Mantle of Mars. Evidence from the Partitioning Behavior of Vanadium in Y980459 (Y98) and Other Olivine-Phyric Shergottites

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.1295s&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.1295

Physics

Scientific paper

Using partitioning behavior of V between olivine and basaltic liquid
precisely calibrated for martian basalts, we determined the redox state
of primitive (olivine-rich, high Mg#) martian basalts near their
liquidus.

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