Cation Distribution Between Forsterite and Metal Alloy at High Temperatures: Implications for the Cooling Rates of Pallasites

Details Cation Distribution Between Forsterite and Metal Alloy at High Temperatures: Implications for the Cooling Rates of Pallasites Cation Distribution Between Forsterite and Metal Alloy at High Temperatures: Implications for the Cooling Rates of Pallasites

Mar 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008lpi....39.1415h&link_type=abstract

39th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXIX), held March 10-14, 2008 in League City, Texas.

Computer Science

Scientific paper

We report metal/olivine partition coefficients for Ni as functions of
temperature, composition and fO2. Such partition coeffients
are essential to interpreting zoning profiles in pallasitic olivines in
terms of cooling rates.

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