Low geomagnetic field strength during End-Cretaceous Deccan volcanism and whole mantle convection

Knowledge about long-term variation of the geomagnetic dipole field remains in its nascent stage because of the paucity of reliable experimental data over geological periods. Here, we present the first robust experimental data from the largest Cretaceous flood basalt province on Earth, the ~65–66 Ma...

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Detalles Bibliográficos
Autores principales: T., Radhakrishna, Mohamed, Asanulla R., M., Venkateshwarlu, S., Soumya G.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7329830/
https://www.ncbi.nlm.nih.gov/pubmed/32612206
http://dx.doi.org/10.1038/s41598-020-67245-6

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7329830/
https://www.ncbi.nlm.nih.gov/pubmed/32612206
http://dx.doi.org/10.1038/s41598-020-67245-6

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