Variable dispersion of Neogene geomagnetic field directions in Iceland

Physics

Scientific paper

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Scientific paper

Analysis of the primary paleomagnetic directions in 4000 lava flows in Iceland reveals that the magnitude of total virtual geomagnetic pole dispersion has decreased during the last 15 Ma. This dispersion, which is independent of the polarity of the field, is in part caused by the occurrence of erratically varying paleofield directions during intermittent periods possibly as long as 100 ka.

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