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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...
| Autores principales: | , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2020
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| Materias: | |
| 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 |