Mass-dependent Oxygen Isotopic Fractionation in Non-FUN Forsterite-bearing Type B CAIs

Details Mass-dependent Oxygen Isotopic Fractionation in Non-FUN Forsterite-bearing Type B CAIs Mass-dependent Oxygen Isotopic Fractionation in Non-FUN Forsterite-bearing Type B CAIs

Mar 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008lpi....39.2039m&link_type=abstract

39th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXIX), held March 10-14, 2008 in League City, Texas.

Computer Science

4

Scientific paper

Four non-FUN forsterite-bearing Type B CAIs show mass-dependent
O-isotopic fractionation related to melt volatilization, but to a lesser
extent than their FUN counterparts. Differences in ambient gas pressure
or precursor compositions are required.

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