Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/3521
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dc.contributor.authorallVizán, H.; Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET) and Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Argentinaen
dc.contributor.authorallVan Zele, M. A.; Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET) and Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Argentinaen
dc.date.accessioned2007-12-31T09:32:21Zen
dc.date.available2007-12-31T09:32:21Zen
dc.date.issued2007-04en
dc.identifier.urihttp://hdl.handle.net/2122/3521en
dc.description.abstractThe main objective of this paper is to show that the distribution of transitional palaeomagnetic data recorded at 250 Ma are in agreement with simulated data that depend on the sampling site, using a model that considers features of the Present Earth magnetic field. The analysis was performed comparing simulated reversals with the Permo-Triassic polarity transition recorded in the Siberian Trap Basalts. The palaeomagnetic data were corrected according to the Palaeo-latitude and Palaeo-longitude of Siberia (absolute reconstruction) at 250 Ma using hotspot tracks. To obtain the motion of Siberia relative to hotspots from the Present time back to 250 Ma, three different Pangaea models were considered (Pangaea A, Pangaea A2, Pangaea B). In spite of the uncertainties associated with the use of hotspot frameworks and Pangaea configurations, both the modelled and recorded data show a remarkable fit when absolute reconstructions of Pangaea A and A2 configurations are performed. The agreement between both simulated and recorded data suggests that similar features to that of the Present Earth magnetic field could have been involved in reversals since the Permo-Triassic.en
dc.language.isoEnglishen
dc.relation.ispartofseries2/50 (2007)en
dc.subjectPermo-Triassicen
dc.subjectPangaeaen
dc.subjectabsolute reconstructionen
dc.subjectEarth magnetic fielden
dc.subjectpolarity transitionen
dc.titleAnalysis of a Permo-Triassic polarity transition in different absolute reconstructions of Pangaea, considering a model with features of the present Earth magnetic fielden
dc.typearticleen
dc.type.QualityControlPeer-revieweden
dc.subject.INGV04. Solid Earth::04.05. Geomagnetism::04.05.02. Geomagnetic field variations and reversalsen
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dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorVizán, H.en
dc.contributor.authorVan Zele, M. A.en
dc.contributor.departmentConsejo Nacional de Investigaciones Científicas y Técnicas (CONICET) and Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Argentinaen
dc.contributor.departmentConsejo Nacional de Investigaciones Científicas y Técnicas (CONICET) and Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Argentinaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptConsejo Nacional de Investigaciones Científicas y Técnicas (CONICET) and Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Argentina-
crisitem.author.deptConsejo Nacional de Investigaciones Científicas y Técnicas (CONICET) and Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Argentina-
crisitem.classification.parent04. Solid Earth-
Appears in Collections:Annals of Geophysics
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