Fe-Isotopic Composition of Chondrules, CAIs, Matrix and Bulk Meteorite in Mokoia and Grosnaja CV-Chondrites

Details Fe-Isotopic Composition of Chondrules, CAIs, Matrix and Bulk Meteorite in Mokoia and Grosnaja CV-Chondrites Fe-Isotopic Composition of Chondrules, CAIs, Matrix and Bulk Meteorite in Mokoia and Grosnaja CV-Chondrites

Mar 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008lpi....39.1603h&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

Chondrules and CAIs in CV chondrites range from -1.40 to +0.21 delta
56Fe. Average chondrule delta 56Fe must be close
to matrix and bulk chondrite. Modeling shows that a combination of
nebula and parent body processes explain the isotopic spread of
chondrules.

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