Constraints on Oxygen Isotopic Evolution from an Amoeboid Olivine Aggregate and Ca,Al-rich Inclusion from the CV3 Efremovka

Details Constraints on Oxygen Isotopic Evolution from an Amoeboid Olivine Aggregate and Ca,Al-rich Inclusion from the CV3 Efremovka Constraints on Oxygen Isotopic Evolution from an Amoeboid Olivine Aggregate and Ca,Al-rich Inclusion from the CV3 Efremovka

Mar 2002

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002lpi....33.1507f&link_type=abstract

33rd Annual Lunar and Planetary Science Conference, March 11-15, 2002, Houston, Texas, abstract no.1507

Computer Science

2

Scientific paper

Primary minerals from an amoeboid olivine aggregate and fine-grained
Ca,Al-rich inclusion from the CV3 Efremovka have 16O-rich
compositions, suggesting that AOAs and most CAIs share a similar source
of oxygen.

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