Saw-toothed pattern of sedimentary paleointensity records explained by cumulative viscous remanence

Details Saw-toothed pattern of sedimentary paleointensity records explained by cumulative viscous remanence Saw-toothed pattern of sedimentary paleointensity records explained by cumulative viscous remanence

Nov 1996

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1996e%26psl.144.....k&link_type=abstract

Earth and Planetary Science Letters, Volume 144, Issue 3-4, p. .

Physics

Scientific paper

The relative paleointensity of the earth's magnetic field from ODP Site 851 has been characterized by progressive decay towards polarity reversals, followed by sharp recovery of pre-reversal values [1]. We resampled the Gilbert-Gauß reversal boundary of this deep-sea core, and show that during demagnetization this `saw-toothed' pattern disappears. Further, the recently published Cumulative Viscous Remanence model [2] using the herewith obtained paleointensity record and constraints from thermal treatment replicates the saw-tooth of [1], implying that it is of non-geomagnetic origin.

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