Do virtual geomagnetic poles follow preferred paths during geomagnetic reversals?
Authors:
- P. L. McFaddenPMP. L. McFadden
- C. E. BartonCBC. E. Barton
- R. T. MerrillRMR. T. Merrill
- 1 January 1993
- journal article
- Published by Springer Nature in Nature
- Vol. 361 (6410) , 342-344
Abstract
No abstract availableKeywords
This publication has 10 references indexed in Scilit:
- Sampling bias in VGP longitudesGeophysical Research Letters, 1992
- Statistical assessment of the preferred longitudinal bands for recent geomagnetic reversal recordsGeophysical Research Letters, 1992
- Dipolar reversal states of the geomagnetic field and core–mantle dynamicsNature, 1992
- Geomagnetic reversal pathsNature, 1992
- Link between geomagnetic reversal paths and secular variation of the field over the past 5 MyrNature, 1992
- Palaeomagnetic constraints on the geometry of the geomagnetic field during reversalsNature, 1992
- Geomagnetic reversal pathsNature, 1991
- A Southern Hemisphere record of the Matuyama‐Brunhes polarity reversalGeophysical Research Letters, 1991
- High-resolution record of the Upper Olduvai transition from Po Valley (Italy) sediments: support for dipolar transition geometry?Physics of the Earth and Planetary Interiors, 1991
- Laboratory studies of depositional DRMGeophysical Journal International, 1980