Late Influx: Evidence from Siderophile Elements in Terrestrial Peridotites and Lunar Breccias

Details Late Influx: Evidence from Siderophile Elements in Terrestrial Peridotites and Lunar Breccias Late Influx: Evidence from Siderophile Elements in Terrestrial Peridotites and Lunar Breccias

Mar 2001

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001lpi....32.1793m&link_type=abstract

32nd Annual Lunar and Planetary Science Conference, March 12-16, 2001, Houston, Texas, abstract no.1793

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Scientific paper

In terrestrial peridotites, Pd is sometimes enhanced relative to other
PGE. This observation is taken to imply a 'non-chondritic' HSE signature
in the mantle. A similar pattern is seen in some Apollo 17 breccias
suggesting it to be a primordial feature of late influx.

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