Overmaturation of Lunar and Mercurian Regolith as a Mechanism of Brightening Effect

Details Overmaturation of Lunar and Mercurian Regolith as a Mechanism of Brightening Effect Overmaturation of Lunar and Mercurian Regolith as a Mechanism of Brightening Effect

Mar 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003lpi....34.1224s&link_type=abstract

34th Annual Lunar and Planetary Science Conference, March 17-21, 2003, League City, Texas, abstract no.1224

Physics

2

Scientific paper

Growth of nanograins of reduced Fe to micron or submicron sizes can
occur at Mercury surface temperatures or in large melted volumes on
Mercury and the Moon. Such growth can result in brightening of mature
regolith ("overmaturation").

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