Mineralogy, Petrography and Oxygen-Isotopic Compositions of Ca, Al-rich Inclusions and Amoeboid Olivine Aggregates in the CR Carbonaceous Chondrites

Details Mineralogy, Petrography and Oxygen-Isotopic Compositions of Ca, Al-rich Inclusions and Amoeboid Olivine Aggregates in the CR Carbonaceous Chondrites Mineralogy, Petrography and Oxygen-Isotopic Compositions of Ca, Al-rich Inclusions and Amoeboid Olivine Aggregates in the CR Carbonaceous Chondrites

Mar 2002

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002lpi....33.1412k&link_type=abstract

33rd Annual Lunar and Planetary Science Conference, March 11-15, 2002, Houston, Texas, abstract no.1412

Mathematics

Logic

3

Scientific paper

CAIs and AOAs in CRs are mineralogically pristine (unaltered). In spite
of the O-isotopic homogeneity of individual CAIs, the compositions of
the CR CAIs and AOAs spread almost continuously over a wide range:
Delta17O = -3‰ - -24‰. All 16O-poor
CAIs have igneous textures.

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