Trace Element Partitioning Between Low-Calcium Pyroxene and Lunar Picritic Glass Melts at Multiple-Saturation Points with Applications to Melting and Melt Migration in A Heterogeneous Lunar Cumulate Mantle

Details Trace Element Partitioning Between Low-Calcium Pyroxene and Lunar Picritic Glass Melts at Multiple-Saturation Points with Applications to Melting and Melt Migration in A Heterogeneous Lunar Cumulate Mantle Trace Element Partitioning Between Low-Calcium Pyroxene and Lunar Picritic Glass Melts at Multiple-Saturation Points with Applications to Melting and Melt Migration in A Heterogeneous Lunar Cumulate Mantle

Mar 2012

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2012lpi....43.1952s&link_type=abstract

43rd Lunar and Planetary Science Conference, held March 19–23, 2012 at The Woodlands, Texas. LPI Contribution No. 1659, id.1952

Computer Science

Scientific paper

Trace-element D values of opx or pigeonite vary by less than a factor of
two for various melt and mineral compositions at multi-saturation
points. We employ a simple model and show the importance of lunar source
composition to mare basalt genesis.

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