Low geomagnetic field strength during End-Cretaceous Deccan volcanism and whole mantle convection
Low geomagnetic field strength during End-Cretaceous Deccan volcanism and whole mantle convection
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London: Nature Publishing Group UK
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English
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London: Nature Publishing Group UK
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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 Deccan basalt within a thick (1250 m) unbiased st...
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Low geomagnetic field strength during End-Cretaceous Deccan volcanism and whole mantle convection
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TN_cdi_doaj_primary_oai_doaj_org_article_a5ee85566fd943c3958cbc97c6e7e9f2
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_a5ee85566fd943c3958cbc97c6e7e9f2
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2045-2322
E-ISSN
2045-2322
DOI
10.1038/s41598-020-67245-6
