Valence State Partitioning of V Between Augite/Melt Crystallized from a Highly Spiked Martian Basalt Composition as a Function of Oxygen Fugacity (IW-1 to FMQ)

Details Valence State Partitioning of V Between Augite/Melt Crystallized from a Highly Spiked Martian Basalt Composition as a Function of Oxygen Fugacity (IW-1 to FMQ) Valence State Partitioning of V Between Augite/Melt Crystallized from a Highly Spiked Martian Basalt Composition as a Function of Oxygen Fugacity (IW-1 to FMQ)

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.1010p&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.1010

Computer Science

1

Scientific paper

This abstract explores the partitioning of vanadium between augite and
melt in a highly-spiked QUE 94201 composition, at each of 4 different
fO2 values (IW-1, IW, IW+1, FMQ).

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