Iron Isotope and the Origin of Nanophase Iron in Lunar Regolith

Details Iron Isotope and the Origin of Nanophase Iron in Lunar Regolith Iron Isotope and the Origin of Nanophase Iron in Lunar Regolith

Mar 2012

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2012lpi....43.1148w&link_type=abstract

43rd Lunar and Planetary Science Conference, held March 19–23, 2012 at The Woodlands, Texas. LPI Contribution No. 1659, id.1148

Computer Science

Scientific paper

We report the iron-isotopic composition of nanophase iron in lunar
regolith. It is highly enriched in heavy isotopes of Fe (δ^5^6Fe
up to 0.71‰). It is due to the preferential loss of light
isotopes to space during vaporization by micrometeorite impacts.

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