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

Jul 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007lpico1353.3013k&link_type=abstract

Seventh International Conference on Mars, held July 9-13, 2007 in Pasadena, California, LPI Contribution No. 1353, p.3013

Physics

Scientific paper

We have inverted global geophysical data for martian composition and
thermal state. The results suggest a mantle enriched in FeO relative to
Earth, but less than the SNCs. We also find a liquid Fe core, ~1600 km
in radius, containing ~12 wt% S, with CMB temperatures around 2350 K.

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