Redox States of Some HED Meteorites as Inferred from Iron Micro-XANES Analyses of Plagioclase

Details Redox States of Some HED Meteorites as Inferred from Iron Micro-XANES Analyses of Plagioclase Redox States of Some HED Meteorites as Inferred from Iron Micro-XANES Analyses of Plagioclase

Mar 2012

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2012lpi....43.1725s&link_type=abstract

43rd Lunar and Planetary Science Conference, held March 19–23, 2012 at The Woodlands, Texas. LPI Contribution No. 1659, id.1725

Physics

Scientific paper

We analyzed plagioclase in HED meteorites by Fe-XANES. The Fe^3^+ ratio
of a cumulate eucrite was high (~0.9), while those of basaltic eucrite
and diogenite were low (~0). This may be related to the heterogeneous
redox environment of Vesta's crust.

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