Constraining the Composition and Thermal State of Mars

Details Constraining the Composition and Thermal State of Mars Constraining the Composition and Thermal State of Mars

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.1283k&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.1283

Physics

Scientific paper

We inverted a set of geophysical data to constrain martian mantle
composition and thermal state. We find a mantle composition similar to
the pyrolite model, except for FeO. For the core, a composition of Fe 14
wt% S and of ~1600 km radius is favoured, while CMB temperatures suggest
it to be fluid.

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