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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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Detalhes bibliográficos
Publicado no:Sci Rep
Main Authors: T., Radhakrishna, Mohamed, Asanulla R., M., Venkateshwarlu, S., Soumya G.
Formato: Artigo
Idioma:Inglês
Publicado em: Nature Publishing Group UK 2020
Assuntos:
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC7329830/
https://ncbi.nlm.nih.gov/pubmed/32612206
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-020-67245-6
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