Controls on Oxygen Fugacity During Martian Basalt Petrogenesis: Clues from Geochemical Correlations

Details Controls on Oxygen Fugacity During Martian Basalt Petrogenesis: Clues from Geochemical Correlations Controls on Oxygen Fugacity During Martian Basalt Petrogenesis: Clues from Geochemical Correlations

Mar 2001

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001lpi....32.1150h&link_type=abstract

32nd Annual Lunar and Planetary Science Conference, March 12-16, 2001, Houston, Texas, abstract no.1150

Physics

1

Scientific paper

The oxygen fugacity of Dar al Gani 476 has been re-evaluated, and is QFM
- 2.3. Oxygen fugacity correlates with geochemical parameters in the
martian basalts, indicative of assimilation of oxidized crustal material
by reduced, mantle-derived melts.

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