Ruthenium isotopic evidence for an inner Solar System origin of the late veneer

Mario Fischer-Gödde () and Thorsten Kleine ()
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Mario Fischer-Gödde: Institut für Planetologie, University of Münster
Thorsten Kleine: Institut für Planetologie, University of Münster

Nature, 2017, vol. 541, issue 7638, 525-527

Abstract: All chondrites are shown to have Ru isotopic compositions that are more different from that of the Earth’s mantle the further from the Sun they formed; this means the Earth’s late veneer cannot derive from volatile-rich material formed in the outer Solar System.

Date: 2017
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DOI: 10.1038/nature21045

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