Hadaean to Palaeoarchaean stagnant-lid tectonics revealed by zircon magnetism

Plate tectonics is a fundamental factor in the sustained habitability of Earth, but its time of onset is unknown, with ages ranging from the Hadaean to Proterozoic eons(1–3). Plate motion is a key diagnostic to distinguish between plate and stagnant-lid tectonics, but palaeomagnetic tests have been...

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Detalles Bibliográficos
Autores principales: Tarduno, John A., Cottrell, Rory D., Bono, Richard K., Rayner, Nicole, Davis, William J., Zhou, Tinghong, Nimmo, Francis, Hofmann, Axel, Jodder, Jaganmoy, Ibañez-Mejia, Mauricio, Watkeys, Michael K., Oda, Hirokuni, Mitra, Gautam
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2023
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10266976/
https://www.ncbi.nlm.nih.gov/pubmed/37316722
http://dx.doi.org/10.1038/s41586-023-06024-5

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10266976/
https://www.ncbi.nlm.nih.gov/pubmed/37316722
http://dx.doi.org/10.1038/s41586-023-06024-5

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