Oxygen Isotopic Compositions of the Al-rich Chondrules in the CR Carbonaceous Chondrites: Evidence for a Genetic Link to Ca-Al-rich Inclusions and for Oxygen Isotope Exchange During Chondrule Melting

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Scientific paper

The Al-rich chondrules in CRs formed by melting of ^16O-rich Ca,Al-rich
precursors, largely composed of anorthite, diopside, and spinel, and
^16O-depleted Fe,Mg-chondrule precursors, and experienced varying
degrees of O-isotope exchange during melting.

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