Constraining the Composition and Thermal State of Mars from Inversion of Geophysical Data

Details Constraining the Composition and Thermal State of Mars from Inversion of Geophysical Data Constraining the Composition and Thermal State of Mars from Inversion of Geophysical Data

Mar 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007lpi....38.1085k&link_type=abstract

38th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXVIII), held March 12-16, 2007 in League City, Texas

Physics

Scientific paper

We have inverted global geophysical for martian composition and thermal
state. Our results suggest a mantle enriched in FeO relative to the
Earth, but less than inferred from the SNC meteorites. We find a liquid
Fe core ~1600 km in radius, containing ~12

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