An Experimental Study of REE Partitioning Between a Dry Shergottite Melt and Pigeonite as a Function of fO2: Implications for the Martian Interior

Details An Experimental Study of REE Partitioning Between a Dry Shergottite Melt and Pigeonite as a Function of fO2: Implications for the Martian Interior An Experimental Study of REE Partitioning Between a Dry Shergottite Melt and Pigeonite as a Function of fO2: Implications for the Martian Interior

Jul 2002

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002m%26psa..37q..97m&link_type=article

Meteoritics & Planetary Science, vol. 37, Supplement, p.A97

Physics

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