Sulfur Solubility in Silicate Melts Saturated with Metal Sulfide at Elevated Pressure and Temperature: Implications for Core-Mantle Interactions

Details Sulfur Solubility in Silicate Melts Saturated with Metal Sulfide at Elevated Pressure and Temperature: Implications for Core-Mantle Interactions Sulfur Solubility in Silicate Melts Saturated with Metal Sulfide at Elevated Pressure and Temperature: Implications for Core-Mantle Interactions

Mar 1999

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1999lpi....30.1013h&link_type=abstract

30th Annual Lunar and Planetary Science Conference, March 15-29, 1999, Houston, TX, abstract no. 1013

Physics

Scientific paper

The bulk silicate Earth's sulfur content is ~7* higher than the expected
sulfur solubility of a silicate liquid. Sulfur-saturated core-forming
metal segregation event is not supported by the expected and observed S
abundances in the Earth's mantle.

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