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Please use this identifier to cite or link to this item: https://cir.cenieh.es/handle/20.500.12136/3282
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dc.contributor.authorPueyo, Emilio L.-
dc.contributor.authorOtaño, Luis-
dc.contributor.authorRoi, Silva-Casal-
dc.contributor.authorCalvín, Pablo-
dc.contributor.authorLaplana, César-
dc.contributor.authorGalindo-Pellicena, María Ángeles-
dc.contributor.authorDuval, Mathieu-
dc.contributor.authorMata, Mª Pilar-
dc.contributor.authorParés, Josep María-
dc.contributor.authorMuñoz, Arsenio-
dc.date.accessioned2024-
dc.date.accessioned2024-07-05T10:58:11Z-
dc.date.issued2024-
dc.identifier.citationEGU General Assembly, 2024, EGU24-8153es_ES
dc.identifier.urihttps://cir.cenieh.es/handle/20.500.12136/3282-
dc.descriptionPonencia presentada en: EGU General Assembly 2024, 14-19 de abril 2024, Viena, Austria & Onlinees_ES
dc.description.abstractThe Porcupine geomagnetic excursion was firstly described at the IODP Site U1308 (North Atlantic). It is a reverse polarity record defined near the top of the Gauss chron (within C2An.1n) and chronostratigraphically constrained between the Kaena and the base of Matuyama reversed chrons. So far, it has been only reported in two different core sections from that site (U1308C-20H-5 and U1308F-20H-2; Channell et al., Q Sci. Rev. 2016). The Porcupine excursion displays a mean age of 2.737 Ma (with an undefined duration) and corresponds to MIS G6 and G7.es_ES
dc.language.isoenes_ES
dc.publisherEuropean Geosciences Union (EGU)es_ES
dc.rightsinfo:eu-repo/semantics/openAccesses_ES
dc.rightsAtribución 3.0 Estados Unidos de América*
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/us/*
dc.titleThe first continental geomagnetic record of an elusive Porcupine?es_ES
dc.typePresentationes_ES
dc.typeOtheres_ES
dc.identifier.doi10.5194/egusphere-egu24-8153-
dc.relation.publisherversionhttps://doi.org/10.5194/egusphere-egu24-8153es_ES
dc.date.available2024-07-05T10:58:11Z-
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