Isotopic evidence for the formation of the Moon in a canonical giant impact

Here, the authors show that Earth and Moon are characterized by different vanadium isotope compositions, which is most likely resulting from vanadium isotope fractionation of the bulk silicate proto-Earth during the main stage of terrestrial core formation—followed by a canonical giant impact scenar...

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Auteurs principaux: Sune G. Nielsen, David V. Bekaert, Maureen Auro
Format: article
Langue:EN
Publié: Nature Portfolio 2021
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Accès en ligne:https://doaj.org/article/ddebb94ca8304d128a0ac601f5578f80
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