Using the Fe/Mn Ratio of FeO-Rich Olivine in Wild 2, Chondrite Matrix, and Type IIA Chondrules to Disentangle Their Histories

Details Using the Fe/Mn Ratio of FeO-Rich Olivine in Wild 2, Chondrite Matrix, and Type IIA Chondrules to Disentangle Their Histories Using the Fe/Mn Ratio of FeO-Rich Olivine in Wild 2, Chondrite Matrix, and Type IIA Chondrules to Disentangle Their Histories

Mar 2012

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2012lpi....43.2748f&link_type=abstract

43rd Lunar and Planetary Science Conference, held March 19–23, 2012 at The Woodlands, Texas. LPI Contribution No. 1659, id.2748

Computer Science

Scientific paper

We compare our data for FeO-rich olivine in matrix and Wild 2 to that of
type IIA chondrules. This comparison yields implications for chondrule
fragmentation, and the mixing and transport of fine-grained material to
the outer solar system.

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