The Influence of Melt Structure on Trace Element Partitioning During Peridotite Partial Melting Beneath Mid-Ocean Ridges at 1.5 GPa

Details The Influence of Melt Structure on Trace Element Partitioning During Peridotite Partial Melting Beneath Mid-Ocean Ridges at 1.5 GPa The Influence of Melt Structure on Trace Element Partitioning During Peridotite Partial Melting Beneath Mid-Ocean Ridges at 1.5 GPa

May 2001

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001eag..conf.3292g&link_type=article

Eleventh Annual V. M. Goldschmidt Conference, May 20-24, 2001, Hot Springs, Virginia, abstract no.3292

Physics

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