Cr Isotope Systematics in the Pallasite Eagle Station: Chronology and Evidence for a Genetic Link to Carbonaceous Chondrites

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Scientific paper

The study of the 53-Mn - 53-Cr system in the pallasite Eagle Station has
shown that it formed 4557.5 +/- 0.6 Ma ago. The Cr isotopic signature is
different from that of the main group pallasites and suggests a genetic
link to CV3 chondrites.

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