Abstract
A decade of modelling Earth's core on computers has led to the belief that we understand what produces Earth's magnetic field. More realistic simulations are now shaking that complacency.
Cite
CITATION STYLE
APA
Christensen, U. R. (2008). A sheet-metal geodynamo. Nature, 454(7208), 1058–1059. https://doi.org/10.1038/4541058a
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