Highly Siderophile Element Abundances and 187Os/188Os in Lunar Impact Melt Rocks: Implications for Late Accretion Processes in the Earth-Moon System

Details Highly Siderophile Element Abundances and 187Os/188Os in Lunar Impact Melt Rocks: Implications for Late Accretion Processes in the Earth-Moon System Highly Siderophile Element Abundances and 187Os/188Os in Lunar Impact Melt Rocks: Implications for Late Accretion Processes in the Earth-Moon System

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.2262f&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.2262

Physics

1

Scientific paper

We report new highly siderophile element abundance and 187Os/188Os data
for lunar impact melt rocks from Apollo 14, 16 and 17 landing sites, and
the lunar meteorite DaG400.

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