Model of geomagnetic paleosecular variations for the Northern Hemisphere

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A model of radial drifting and oscillating dipoles to represent geomagnetic palaeosecular variations, which showed to be appropriate for the Southern Hemisphere, is evaluated for the Northern Hemisphere. After a new fitting of some involved parameters, its theoretical results are compared with the p...

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Autor principal: Sinito, Ana María
Otros Autores: Vilas, J.F
Formato: Capítulo de libro
Lenguaje:Inglés
Publicado: Kluwer Academic Publishers 1991
Acceso en línea:Registro en Scopus
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100 1 |a Sinito, Ana María 
245 1 0 |a Model of geomagnetic paleosecular variations for the Northern Hemisphere 
260 |b Kluwer Academic Publishers  |c 1991 
270 1 0 |m Sinito, A.M.; Consefo Nacional de Investigaciones Cientificas y Tecnicas and Universidad de Buenos AiresArgentina 
504 |a Gauss, C.F., Allgemeine Theorie des Erdmagnetismus (1839) Resultate aus den Beobachtungen des magnetischen Vereins in Jahre, 1838, p. 1 
504 |a Lowes, F.J., Runcorn, G., The analysis of the geomagnetic secular variation (1951) Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 243, p. 525 
504 |a Bochev, A.Z., Presenting the Earth's magnetic field as a field of six optimal dipoles (1975) C. R. Acad. Bulgare Sci., 28, p. 569 
504 |a Alldredge, L.R., Hurwitz, L., Radial dipoles as the source of the Earth's main magnetic field (1964) J. Geoph. Res., 69, p. 12 
504 |a Creer, K.M., Geomagnetic secular variation during the last 25 000 years: an interpretation of data obtained from rapidly deposited sediments (1977) Geophysical Journal International, 48, p. 91 
504 |a Peddie, N., Current loop models of the Earth's magnetic field (1979) J. Geophys. Res., 84 (9 B), p. 4517 
504 |a T. E. Hogg: The Holocene geomagnetic field in Europe. Thesis, University of Edinburgh 1978; Creer, K.M., Computer synthesis of geomagnetic palaeosecular variations (1983) Nature, 304, p. 695 
504 |a A. M. Sinito: Análisis de las variaciones geomagnéticas paleoseculares recientes en el Hemisferio Sur z su relación con los modelos fisicos que postulan el origen del campo magnético terrestre. Thesis, Universidad de Buenos Aires 1988; Sinito, A.M., Models of geomagnetic secular variations on recent times for South America (1990) Phys. Earth Planet. Interiors, 64, p. 133 
504 |a G. Smith: Late Glacial Paleomagnetic Secular Variations from France. Ph. D. thesis, University of Edinburgh 1985; Smith, G., Creer, K.M., Analysis of geomagnetic secular variations 10 000 to 30 000 years bp, Lac du Bouchet, France (1986) Phys. Earth Planet. Interiors, 44, p. 1 
504 |a Creer, K.M., Geomagnetic variations for the interval 7,000–25,000 yr B.P. as recorded in a core of sediment from station 1474 of the Black Sea Cruise of “Atlantis II” (1974) Earth Planet. Sci. Lett., 23, p. 34 
504 |a A. M. Sinito, J. F. Vilas: Palaeosecular variations models for the interval 0–10 000 years bp for Southern Hemisphere. 6th Scientific Assembly IAGA, Exeter, U. K. Abstract, (1989) B, 135; Creer, K.M., Valencio, D.A., Valencio, A.M., Tucholka, P., Vilas, J.F., Geomagnetic secular variation 0–14 000 yr BP as recorded by lake sediments from Argentina (1983) Geophys. J. R. Astr. Soc., 74, p. 199 
504 |a Barton, C.L., McElhinny, M.W., A 10 000 years geomagnetic secular variation record from three Australian Maars (1981) Geophys. J. R. Astr. Soc., 67, p. 465 
504 |a Denham, C.R., Spectral analysis of paleomagnetic time series techniques and applications (1975) Journal of Geophysical Research, 80, p. 1897 
504 |a Rao, C.R., Mitra, J.K., Matthai, A., (1966) Formulae and tables for statistical work, , Statistical Publishing Society, Calcutta 
506 |2 openaire  |e Política editorial 
520 3 |a A model of radial drifting and oscillating dipoles to represent geomagnetic palaeosecular variations, which showed to be appropriate for the Southern Hemisphere, is evaluated for the Northern Hemisphere. After a new fitting of some involved parameters, its theoretical results are compared with the palaeomagnetic data of Lake de Bouchet (France) and the Black Sea. A time lag between the declination and inclination profiles is observed in both cases. A good cross-correlation coefficient is obtained for the declination and inclination data. © 1991 ACADEMIA, Publishing House of the Czechoslovak Academy of Sciences.  |l eng 
593 |a Consefo Nacional de Investigaciones Cientificas y Tecnicas and Universidad de Buenos Aires, Argentina 
593 |a Facultad de Ciencias Exactas y Naturales, Departamento de Ciencias Geologicas, Laboratorio de Paleomagnetismo, Ciudad Universitaria, Pab. 2, Buenos Aires, 1428, Argentina 
700 1 |a Vilas, J.F. 
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856 4 0 |u https://doi.org/10.1007/BF01613979  |y DOI 
856 4 0 |u https://hdl.handle.net/20.500.12110/paper_00393169_v35_n4_p334_Sinito  |y Handle 
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