Fe-Mg Partitioning Between Olivine and Martian Magmas: Application to Genesis of Olivine-Phyric Shergottites and Conditions of Melting in the Martian Interior

Details Fe-Mg Partitioning Between Olivine and Martian Magmas: Application to Genesis of Olivine-Phyric Shergottites and Conditions of Melting in the Martian Interior Fe-Mg Partitioning Between Olivine and Martian Magmas: Application to Genesis of Olivine-Phyric Shergottites and Conditions of Melting in the Martian Interior

Sep 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010m%26psa..73.5295f&link_type=article

73rd Annual Meeting of the Meteoritical Society, held July 26-30, 2010 in New York, New York. Published in Meteoritics and Plane

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