Partition coefficients for Al, Ca, Ti, Cr, and NI in olivine obtained by melting experiment on an LL6 chondrite

Details Partition coefficients for Al, Ca, Ti, Cr, and NI in olivine obtained by melting experiment on an LL6 chondrite Partition coefficients for Al, Ca, Ti, Cr, and NI in olivine obtained by melting experiment on an LL6 chondrite

Mar 1994

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1994lpi....25..923m&link_type=abstract

In Lunar and Planetary Inst., The Twenty-Fifth Lunar and Planetary Science Conference. Part 2: H-O p 923-924 (SEE N94-36136 11-9

Mathematics

Aluminum, Calcium, Chondrites, Chromium, Coefficients, Melting, Meteoritic Composition, Nickel, Olivine, Partitions (Mathematics), Titanium, Oxygen, Temperature Effects

Scientific paper

We report the partition coefficients for Ca, Al, Ti, Cr, and Ni in olivine obtained through a series of melting experiments on an LL6 chondrite under varying conditions of temperature and oxygen fugacity. It is necessary to examine the variation of partition coefficients up to extremely reducing conditions in order to study meteoritic olivines. For Ca, Al, and Cr, the partition coefficients tend to decrease as temperature increases, but do not change even under extremely reducing conditions.

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