Early Cambrian renewal of the geodynamo and the origin of inner core structure

Paleomagnetism can elucidate the origin of inner core structure by establishing when crystallization started. The salient signal is an ultralow field strength, associated with waning thermal energy to power the geodynamo from core-mantle heat flux, followed by a sharp intensity increase as new therm...

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Detalles Bibliográficos
Autores principales: Zhou, Tinghong, Tarduno, John A., Nimmo, Francis, Cottrell, Rory D., Bono, Richard K., Ibanez-Mejia, Mauricio, Huang, Wentao, Hamilton, Matt, Kodama, Kenneth, Smirnov, Aleksey V., Crummins, Ben, Padgett, Frank
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9296475/
https://www.ncbi.nlm.nih.gov/pubmed/35853855
http://dx.doi.org/10.1038/s41467-022-31677-7

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9296475/
https://www.ncbi.nlm.nih.gov/pubmed/35853855
http://dx.doi.org/10.1038/s41467-022-31677-7

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