Modification of the Iron Mineralogy, Chemistry and Isotopic Composition of H5 and L6 Ordinary Chondrites During Desertic Weathering

Details Modification of the Iron Mineralogy, Chemistry and Isotopic Composition of H5 and L6 Ordinary Chondrites During Desertic Weathering Modification of the Iron Mineralogy, Chemistry and Isotopic Composition of H5 and L6 Ordinary Chondrites During Desertic Weathering

Mar 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008lpi....39.1534s&link_type=abstract

39th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXIX), held March 10-14, 2008 in League City, Texas.

Physics

Scientific paper

Ordinary chondrites from hot deserts are affected by terrestrial
weathering that modifies their mineralogy and geochemistry. This also
leads to increasing iron isotope signatures corresponding to the
preferential retention of isotopically heavy, oxidized iron.

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