Fingerprinting the Cretaceous-Paleogene boundary impact with Zn isotopes
Elevated Zn isotope compositions occur in K-Pg sedimentary layers of three different depositional environments across North America and the Caribbean. The data indicate a volatilization event, and act as a robust mechanistic indicator of the meteorite impact at the end of the Cretaceous.
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Autores principales: | , , , , , , , , |
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Formato: | article |
Lenguaje: | EN |
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Nature Portfolio
2021
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Acceso en línea: | https://doaj.org/article/2e27242bfcc946d7a4e77849a224aa54 |
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