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Cited by 213

The DOI matches its Crossref record; 3 of the 3 references it cites were found in a registry or an index.

Earth's Core and the Geodynamo

Buffett, Bruce A.·2000·Science

Abstract

Earth's magnetic field is generated by fluid motion in the liquid iron core. Details of how this occurs are now emerging from numerical simulations that achieve a self-sustaining magnetic field. Early results predict a dominant dipole field outside the core, and some models even reproduce magnetic reversals. The simulations also show how different patterns of flow can produce similar external fields. Efforts to distinguish between the various possibilities appeal to observations of the time-dependent behavior of the field. Important constraints will come from geological records of the magnetic field in the past.

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Metadata

Authors
Buffett, B. A.
Venue
Science
Published
2000-06-16
Volume
288
Issue
5473
Pages
2007-2012
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2055992533
Cited by
213
References
3
FWCI
1.92
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Earth's Core and the Geodynamo. https://app.cochat.ai/papers/10.1126/science.288.5473.2007
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Buffett, B. A. (2000). Earth's Core and the Geodynamo. Science. https://doi.org/10.1126/science.288.5473.2007

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.