Partitioning of Ni, Co, Sc, La, and other Elements Between Olivine and Natural Basaltic Melt at 75 Kbars and 1800 deg C, and Implications for the Early Thermal History of the Earth

Details Partitioning of Ni, Co, Sc, La, and other Elements Between Olivine and Natural Basaltic Melt at 75 Kbars and 1800 deg C, and Implications for the Early Thermal History of the Earth Partitioning of Ni, Co, Sc, La, and other Elements Between Olivine and Natural Basaltic Melt at 75 Kbars and 1800 deg C, and Implications for the Early Thermal History of the Earth

Mar 1989

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1989lpi....20..662m&link_type=gif

Abstracts of the Lunar and Planetary Science Conference, volume 20, page 662, (1989)

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