Model of geomagnetic paleosecular variations for the Northern Hemisphere

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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Autores principales: Sinito, A.M., Vilas, J.F.
Formato: JOUR
Acceso en línea:http://hdl.handle.net/20.500.12110/paper_00393169_v35_n4_p334_Sinito
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Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires
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spelling todo:paper_00393169_v35_n4_p334_Sinito2023-10-03T14:49:35Z Model of geomagnetic paleosecular variations for the Northern Hemisphere Sinito, A.M. Vilas, J.F. 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. Fil:Sinito, A.M. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Vilas, J.F. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_00393169_v35_n4_p334_Sinito
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
description 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.
format JOUR
author Sinito, A.M.
Vilas, J.F.
spellingShingle Sinito, A.M.
Vilas, J.F.
Model of geomagnetic paleosecular variations for the Northern Hemisphere
author_facet Sinito, A.M.
Vilas, J.F.
author_sort Sinito, A.M.
title Model of geomagnetic paleosecular variations for the Northern Hemisphere
title_short Model of geomagnetic paleosecular variations for the Northern Hemisphere
title_full Model of geomagnetic paleosecular variations for the Northern Hemisphere
title_fullStr Model of geomagnetic paleosecular variations for the Northern Hemisphere
title_full_unstemmed Model of geomagnetic paleosecular variations for the Northern Hemisphere
title_sort model of geomagnetic paleosecular variations for the northern hemisphere
url http://hdl.handle.net/20.500.12110/paper_00393169_v35_n4_p334_Sinito
work_keys_str_mv AT sinitoam modelofgeomagneticpaleosecularvariationsforthenorthernhemisphere
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