SAW-TOOTHED PATTERN OF SEDIMENTARY PALEOINTENSITY RECORDS EXPLAINED BY CUMULATIVE VISCOUS REMANENCE

dc.contributor.author	Kok Y.S.
dc.contributor.author	Tauxe L.
dc.date.accessioned	2020-11-21T07:53:53Z
dc.date.available	2020-11-21T07:53:53Z
dc.date.issued	1996
dc.identifier	https://elibrary.ru/item.asp?id=488766
dc.identifier.citation	Earth and Planetary Science Letters, 1996, , 3, E9-E14
dc.identifier.issn	0012-821X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/19221
dc.description.abstract	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-Gausz 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.
dc.subject	VISCOUS REMANENT MAGNETIZATION
dc.subject	PALEOMAGNETISM
dc.subject	GILBERT EPOCH
dc.subject	GAUSS EPOCH
dc.subject	REVERSALS
dc.subject	MAGNETIC FIELD
dc.title	SAW-TOOTHED PATTERN OF SEDIMENTARY PALEOINTENSITY RECORDS EXPLAINED BY CUMULATIVE VISCOUS REMANENCE
dc.type	Статья

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