The "Late Veneer" on Earth: Evidence from Eoarchean Ultramafic Schists (Metakomatiites)

Details The "Late Veneer" on Earth: Evidence from Eoarchean Ultramafic Schists (Metakomatiites) The "Late Veneer" on Earth: Evidence from Eoarchean Ultramafic Schists (Metakomatiites)

Mar 2012

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2012lpi....43.2890f&link_type=abstract

43rd Lunar and Planetary Science Conference, held March 19–23, 2012 at The Woodlands, Texas. LPI Contribution No. 1659, id.2890

Physics

Scientific paper

Contemporary peridotites show an enhanced concentration of the highly
siderophile elements (HSEs). This is believed to be due to a late
accretion event called the Late Veneer. Here we show the evolution of
the HSE signature using ancient komatiites.

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