The Formation of Type II Chondrules in CM Chondrites: The View from Paris

Details The Formation of Type II Chondrules in CM Chondrites: The View from Paris The Formation of Type II Chondrules in CM Chondrites: The View from Paris

Mar 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011lpi....42.1914h&link_type=abstract

42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas. LPI Contribution No. 1608, p.1914

Physics

Scientific paper

In Paris (CM) Type II chondrules, olivine cores are Fa7-76 with
Fa1-19 relics. Fe-Mn correlations show that CM and LL chondrules
come from different reservoirs and formed by condensation of Fe and Mn
onto Type I material in a late oxidizing environment.

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