High Geomagnetic Intensity during the Mid-Cretaceous from Thellier Analyses of Single Plagioclase Crystals
Recent numerical simulations have yielded the most efficient geodynamo, having the largest dipole intensity when reversal frequency is low. Reliable paleointensity data are limited but heretofore have suggested that reversal frequency and paleointensity are decoupled. We report data from 56 Thellier...
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Veröffentlicht in: | Science (American Association for the Advancement of Science) 2001-03, Vol.291 (5509), p.1779-1783 |
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