Experimental Constraints on the Stability of Clinopyroxene + Magnesite in Iron Bearing Planetary Mantles: Implications for Nakhlite Formation

Details Experimental Constraints on the Stability of Clinopyroxene + Magnesite in Iron Bearing Planetary Mantles: Implications for Nakhlite Formation Experimental Constraints on the Stability of Clinopyroxene + Magnesite in Iron Bearing Planetary Mantles: Implications for Nakhlite Formation

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.2419m&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.2419

Computer Science

Scientific paper

We performed experiments on Fe/C interactions in planetary mantles.
Melting of magnesite + clinopyroxene at 1.8 GPa-1100 to
1300˚C produces a CaO-, CO2-rich melt in equilibrium with olivine
and cpx that have similar compositions as nakhlite minerals.

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