Experimental Constraints on the Iron Content of the Martian Mantle

Details Experimental Constraints on the Iron Content of the Martian Mantle Experimental Constraints on the Iron Content of the Martian Mantle

Mar 2004

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004lpi....35.1880a&link_type=abstract

35th Lunar and Planetary Science Conference, March 15-19, 2004, League City, Texas, abstract no.1880

Computer Science

Scientific paper

FeO/MnO trends of basaltic shergottites, chondrites, and high pressure
partial melts of L-chondrite suggest that the Martian mantle composition
is similar to H-chondrites with Mg#~80. We are currently testing this
hypothesis through high pressure experiments on the Farmville H4
chondrite.

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