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Kenneth A. Hoffman and Nobutatsu Mochizuki Evidence of a partitioned dynamo reversal process from paleomagnetic recordings in Tahitian lavas Geophysical Research Letters 39

Version of Record online: 27 MAR 2012 | DOI: 10.1029/2011GL050830

Key Points

  • Axial dipole and flux in the shallow core reverse quasi-independently
  • Two-stage geodynamo reversal process, possibly due to stratification
  • Supports contention of a long-held influence over pattern by lower-most mantle

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