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.
Citation Information
| Publication Year | 1985 |
|---|---|
| Title | How the geomagnetic field vector reverses polarity |
| DOI | 10.1038/316230a0 |
| Authors | M. Prevot, E. A. Mankinen, C.S. Grommé, R. S. Coe |
| Publication Type | Article |
| Publication Subtype | Journal Article |
| Series Title | Nature |
| Index ID | 70013010 |
| Record Source | USGS Publications Warehouse |