Sulfide Undersaturated Apollo 12 Basaltic Magmas: Implications for Chalcophile Element Abundance in the Lunar Mantle

Details Sulfide Undersaturated Apollo 12 Basaltic Magmas: Implications for Chalcophile Element Abundance in the Lunar Mantle Sulfide Undersaturated Apollo 12 Basaltic Magmas: Implications for Chalcophile Element Abundance in the Lunar Mantle

Mar 2002

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002lpi....33.1177b&link_type=abstract

33rd Annual Lunar and Planetary Science Conference, March 11-15, 2002, Houston, Texas, abstract no.1177

Physics

Scientific paper

Sulfur contents of homogenized, olivine-hosted melt inclusions from A12
picritic basalts show that the magma was undersaturated in sulfide. Low
chalcophile element abundances in mare basalts must be a primary feature
of the lunar mantle and not due to residual sulfide during melting.

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