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- W2186550800 abstract "The Geomagnetic field can be described mainly as the field developed by a geocentric axial dipole and this property is at the core of successful applications of paleomagnetism to tectonics. The study of the spatial and temporal characteristics of the secular variation of the geomagnetic field is important to understand its origin. The uneven geographic distribution of paleomagnetic results with few available data in the southern hemisphere, however, impedes an accurate analysis of the fine-scale changes in the statistical characteristics of paleosecular variations [See Jacobs, 19941 . The behavior of the earth magnetic field during polarity reversal has also been recently the subject of large debate on a possible confining of transitional field paths over specific longitudinal bands and it is interpreted as evidence for core-mantle interaction [Gubbins, 19941." @default.
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- W2186550800 date "1996-01-01" @default.
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- W2186550800 title "PRELIMINARY PALEOMAGNETIC RESULTS FROM THE PLEISTOCENE VILLARICA VOLCANO AND MIOCENE FARELLONES FORMATION" @default.
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