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Paleomagnetism in speleothems: influence of calcite growth dip on the natural remanent magnetization

2016Journal article Open access
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dc.contributor.authorFont, E.
dc.contributor.authorPonte, J.
dc.contributor.authorVeiga-Pires, C.
dc.contributor.authorHillaire-Marcel, C.
dc.date.accessioned2017-03-31T20:14:49Z
dc.date.available2017-03-31T20:14:49Z
dc.date.issued2016
dc.date.updated2017-03-30T00:05:09Z
dc.description.abstractRecent studies recognized speleothems as excellent recorders of the Earth’s magnetic field. However, some questions remain about the origin of the natural remanent magnetization and about the influence of the speleothem shape on the recorded magnetic directions.pt_PT
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.citationFont, E.; Ponte, J.; Veiga-Pires, Cristina Carvalho; Hillaire-Marcel, C.Paleomagnetism in speleothems: Influence of calcite growth dip on the natural remanent magnetization, Trabalho apresentado em EGU, In Geophysical Research Abstracts , Vienna, 2016.pt_PT
dc.identifier.otherAUT: CVP01371;
dc.identifier.urihttp://hdl.handle.net/10400.1/9130
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.publisherEuropean Geosciences Unionpt_PT
dc.titlePaleomagnetism in speleothems: influence of calcite growth dip on the natural remanent magnetizationpt_PT
dc.typejournal article
dspace.entity.typePublication
oaire.citation.titleEGU, Geophysical Research Abstractspt_PT
oaire.citation.volume18pt_PT
person.familyNameVeiga-Pires
person.givenNameCristina
person.identifier113325
person.identifier.ciencia-id4A1F-CEDA-E66C
person.identifier.orcid0000-0002-9323-0723
person.identifier.ridB-5144-2008
person.identifier.scopus-author-id7801372905
rcaap.rightsopenAccesspt_PT
rcaap.typearticlept_PT
relation.isAuthorOfPublicationd1541efa-0eaa-48dc-aea3-a1e64aa0065a
relation.isAuthorOfPublication.latestForDiscoveryd1541efa-0eaa-48dc-aea3-a1e64aa0065a

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