Partitioning of W Between Liquid Metal, Solid Silicates, and Liquid Silicates at High Pressures and Temperatures: Implications for the 182W Isotope Anomalies in Lunar and Martian Samples

Details Partitioning of W Between Liquid Metal, Solid Silicates, and Liquid Silicates at High Pressures and Temperatures: Implications for the 182W Isotope Anomalies in Lunar and Martian Samples Partitioning of W Between Liquid Metal, Solid Silicates, and Liquid Silicates at High Pressures and Temperatures: Implications for the 182W Isotope Anomalies in Lunar and Martian Samples

Mar 1999

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1999lpi....30.1381r&link_type=abstract

30th Annual Lunar and Planetary Science Conference, March 15-29, 1999, Houston, TX, abstract no. 1381

Physics

Scientific paper

New high pressure and temperature experiments on partially molten basalt
and chondrite show that the 182W anomalies measured in lunar and martian
samples must be interpreted with a full undertsanding of metal-silicate
and clinopyroxene-silicate liquid partitioning.

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