Extending the Solidus for a Model Iron-rich Martian Mantle Composition to 25 GPa

Details Extending the Solidus for a Model Iron-rich Martian Mantle Composition to 25 GPa Extending the Solidus for a Model Iron-rich Martian Mantle Composition to 25 GPa

Mar 2001

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001lpi....32.1157s&link_type=abstract

32nd Annual Lunar and Planetary Science Conference, March 12-16, 2001, Houston, Texas, abstract no.1157

Computer Science

Scientific paper

Multianvil experiments utilizing a model anhydrous Martian mantle
composition were used to determine the solidus. This study provides
solidus data for this model composition at the mid-mantle (15 GPa) to
core/mantle boundary (25 GPa) of Mars.

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