Petrologic-Isotopic Study of Amoeboid Olivine Aggregates in CR Chondrites

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Scientific paper

We report O and Mg isotopic compositions of minerals in CR AOAs.
Minerals in AOAs are 16O-rich. Refractory minerals in CR AOAs have 26Mg
excesses and initial 26Al values as high as CAIs. They have initial
26Al/27Al ratios comparable to canonical values an

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