Low geomagnetic field strength during End-Cretaceous Deccan volcanism and whole mantle convection
Abstract 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...
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Auteurs principaux: | , , , |
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Format: | article |
Langue: | EN |
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Nature Portfolio
2020
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Accès en ligne: | https://doaj.org/article/a5ee85566fd943c3958cbc97c6e7e9f2 |
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