Iron Isotope Evidence for Formation of the Moon Through Partial Vaporisation

Details Iron Isotope Evidence for Formation of the Moon Through Partial Vaporisation Iron Isotope Evidence for Formation of the Moon Through Partial Vaporisation

Mar 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003lpi....34.1433p&link_type=abstract

34th Annual Lunar and Planetary Science Conference, March 17-21, 2003, League City, Texas, abstract no.1433

Computer Science

1

Scientific paper

The isotopic composition of iron in lunar samples is heavy relative to
the Earth, which is itself heavier than meteorites from Mars and Vesta.
This may be the imprint of planetary partial vaporisation during the
Giant Impact that led to the formation of the Moon.

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