Molybdenum Metal-Silicate Partitioning Behavior: Constraining the Magma Ocean Hypothesis for Core Formation

Details Molybdenum Metal-Silicate Partitioning Behavior: Constraining the Magma Ocean Hypothesis for Core Formation Molybdenum Metal-Silicate Partitioning Behavior: Constraining the Magma Ocean Hypothesis for Core Formation

Mar 2012

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2012lpi....43.2155b&link_type=abstract

43rd Lunar and Planetary Science Conference, held March 19–23, 2012 at The Woodlands, Texas. LPI Contribution No. 1659, id.2155

Computer Science

Scientific paper

Mo metal-silicate partitioning experiments were performed over a P range
of 3-20 GPa and a T range of 2173-2673 K. Parameterization
of our new data and literature data indicates Mo is compatible with the
deep (42-57 GPa) magma ocean hypothesis.

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