A More Reduced Mantle Source for Enriched Shergottites; Insights from Olivine-Phyric Shergottite LAR 06319

Details A More Reduced Mantle Source for Enriched Shergottites; Insights from Olivine-Phyric Shergottite LAR 06319 A More Reduced Mantle Source for Enriched Shergottites; Insights from Olivine-Phyric Shergottite LAR 06319

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.1503p&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.1503

Physics

Scientific paper

LAR 06319 detailed oxybarometry shows that a basaltic melt becomes more
oxidized during differentiation. The first crystallized assemblages are
used to redefine the oxygen fugacity of the enriched shergottite mantle
source to the value of FMQ-2.

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