| Abstract: | A highly detailed record of both the direction and intensity of the Earth‘s magnetic field as it reverses has been obtained from a Miocene volcanic sequence. The transitional field is low in intensity and is typically non-axisymmetric. Geomagnetic impulses corresponding to astonishingly high rates of change of the field sometimes occur, suggesting that liquid velocity within the Earth‘s core increases during geomagnetic reversals. ?? 1985 Nature Publishing Group. |
| Genre: | Article |
| ProdID: | 70013010 |
| Citation Author: | Prevot, M.; Mankinen, E. A.; Gromme, C. S.; Coe, R. S. |
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| Citation End Page: | 234 |
| Citation Issue: | 6025 |
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| Citation Language: | English |
| Citation Larger Work Title: | Nature |
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| Citation Number Of Pages: | 5 |
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| Citation Search Results Text: | How the geomagnetic field vector reverses polarity; 1985; Article; Journal; Nature; Prevot, M.; Mankinen, E. A.; Gromme, C. S.; Coe, R. S. |
| Citation Start Page: | 230 |
| Citation Volume: | 316 |
| Citation Year: | 1985 |
| Type: | citation/reference |
| Text: | How the geomagnetic field vector reverses polarity; 1985; Article; Journal; Nature; Prevot, M.; Mankinen, E. A.; Gromme, C. S.; Coe, R. S. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| URL (DIGITAL OBJECT IDENTIFIER): | http://dx.doi.org/10.1038/316230a0 |
| Date Other: | Tue, 1 Jan 1985 00:00 -0600 |
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