Please use this identifier to cite or link to this item: http://hdl.handle.net/20.500.12136/1827
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dc.contributor.authorSier, Mark Jan-
dc.contributor.authorPeeters, Jan-
dc.contributor.authorDekkers, Mark‏ J.-
dc.contributor.authorBusschers, Freek Sander-
dc.contributor.authorParés, Josep María-
dc.contributor.authorBunnik, Frans-
dc.contributor.authorRoebroeks, Wil-
dc.date.accessioned2020-04-
dc.date.accessioned2020-04-17T15:08:59Z-
dc.date.issued2012-
dc.identifier.citationINQUA SEQS 2012 Meeting. At the edge of the aea: sediments, geomorphology, tectonics, and stratigraphy in quaternary studies, 2012, p. 89es_ES
dc.identifier.urihttp://hdl.handle.net/20.500.12136/1827-
dc.descriptionPonencia presentada: INQUA SEQS 2012 Meeting. At the edge of the aea: sediments, geomorphology, tectonics, and stratigraphy in quaternary studies: Sardinia, Italy, 26-27 september, 2012es_ES
dc.language.isoenes_ES
dc.publisherInternational Union for Quaternary Researches_ES
dc.rightsinfo:eu-repo/semantics/openAccesses_ES
dc.titleA palaeomagnetic signal from the Last Interglaciales_ES
dc.typePresentationes_ES
dc.typeOtheres_ES
dc.date.available2020-04-17T15:08:59Z-
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