An Experimental Investigation of the Pressure Effect on Stable Isotope Fractionation at High Temperature; Implications for Mantle Processes and Core Formation in Celestial Bodies from 1 GPa and Up to 25 Gpa

Details An Experimental Investigation of the Pressure Effect on Stable Isotope Fractionation at High Temperature; Implications for Mantle Processes and Core Formation in Celestial Bodies from 1 GPa and Up to 25 Gpa An Experimental Investigation of the Pressure Effect on Stable Isotope Fractionation at High Temperature; Implications for Mantle Processes and Core Formation in Celestial Bodies from 1 GPa and Up to 25 Gpa

Mar 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011lpi....42.1376m&link_type=abstract

42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas. LPI Contribution No. 1608, p.1376

Computer Science

Scientific paper

We show how the stable isotope ratios observed in primary mantle
minerals from celestial bodies may not reflect their source composition
and how during core formation the depth of equilibration can play a
major role in fractionation up to 25 GPa.

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