Long-range dependence in the Cenozoic reversal record

Details Long-range dependence in the Cenozoic reversal record Long-range dependence in the Cenozoic reversal record

Mar 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003pepi..135..253j&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 135, Issue 4, p. 253-266.

Physics

18

Scientific paper

The frequency distribution of intervals between Cenozoic geomagnetic reversals approximates a power law, while their occurrence over time shows temporal clustering of short and long intervals. Application of the Aggregate Variance and Absolute Value methods suggest long-range dependence in this time series, a possible indication that the geodynamo operates as a self-organised complex system. This hypothesis may allow the Cretaceous superchron to be considered as an integral part of the ordinary reversal regime attested in the Cenozoic record.

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