Oxygen Isotopic Compositions of Chondrule Glasses in Semarkona (LL3.0): Search for 16O-depleted Components in Chondrules

Details Oxygen Isotopic Compositions of Chondrule Glasses in Semarkona (LL3.0): Search for 16O-depleted Components in Chondrules Oxygen Isotopic Compositions of Chondrule Glasses in Semarkona (LL3.0): Search for 16O-depleted Components in Chondrules

Mar 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007lpi....38.1791k&link_type=abstract

38th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXVIII), held March 12-16, 2007 in League City, Texas

Physics

3

Scientific paper

We found variable amount of capital delta-17O in chondrule glasses up to
+5?, though they are much higher than coexisting clino-pyroxene. The
result implies oxygen isotope exchange with 16O depleted nebula gas
during chondrule formation was limited.

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