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dc.contributor.authorPorquet, Manuel
dc.contributor.authorPueyo, Emilio L.
dc.contributor.authorRomán Berdiel, Teresa
dc.contributor.authorOlivier, Philippe
dc.contributor.authorLongares Aladrén, Luis A.
dc.contributor.authorCuevas Urionabarrenechea, Julia
dc.contributor.authorRamajo, Javier
dc.contributor.authorAntolín, Borja
dc.contributor.authorAranguren Iriarte, Aitor
dc.contributor.authorAurejac, Jean Baptiste
dc.contributor.authorBouchez, Jean-Luc
dc.contributor.authorCasas, Antonio M.
dc.contributor.authorDenèlee, Yoann
dc.contributor.authorGleizese, Gerard
dc.contributor.authorHilario, Asier
dc.contributor.authorIzquierdo Llavallc, Esther
dc.contributor.authorLeblanc, Dennis
dc.contributor.authorOliva Urcia, Belén
dc.contributor.authorSantana, Vicente
dc.contributor.authorTubía Martínez, José María
dc.contributor.authorVegas Tubia, Néstor
dc.date.accessioned2025-01-21T17:38:09Z
dc.date.available2025-01-21T17:38:09Z
dc.date.issued2017
dc.identifier.citationJournal of Maps 13(2) : 438-448 (2017)es_ES
dc.identifier.issn1744-5647
dc.identifier.urihttp://hdl.handle.net/10810/71678
dc.description.abstract[EN]In this paper, we report on a compilation of more than 2200 sites (more than 10,000 individual measurements) where anisotropy of magnetic susceptibility (AMS) was studied in granites from the Variscan Pyrenees. The standardization and homogenization of this information has allowed us to produce three Main Maps that synthesize all the information related with the AMS of the Pyrenean granites. We also describe the problems found during the construction of the database (variable geo-positioning, different published information, etc.). The information derived from 21 granite bodies, the database, and the synthesis maps (magnetic susceptibility, Km, and the orientation of the magnetic foliation, plane perpendicular to k3, and of the magnetic lineation, k1) allow us to see for the first time a complete image of this important kinematic and petrographic indicator.es_ES
dc.description.sponsorshipThis work was founded by the projects DR3AM (CGL2014– 55118), PmagIGME and GeoPyrDatabases (PI165/09) financed by the MINECO, IGME and the Aragonian Gov- ernment, respectively.es_ES
dc.language.isospaes_ES
dc.publisherTaylor & Francises_ES
dc.rightsinfo:eu-repo/semantics/openAccesses_ES
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/*
dc.subjectAMSes_ES
dc.subjectVariscan Pyreneeses_ES
dc.subjectmagnetic lineationes_ES
dc.subjectmagnetic foliationes_ES
dc.subjectbulk susceptibilityes_ES
dc.subjectgranitoides_ES
dc.titleAnisotropy of magnetic susceptibility of the Pyrenean graniteses_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.holder© 2017 The Author(s). Published by Informa UK Limited, trading as Taylor & Francis Group on behalf of Journal of Maps This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.es_ES
dc.relation.publisherversionhttps://www.tandfonline.com/doi/full/10.1080/17445647.2017.1302364es_ES
dc.identifier.doi10.1080/17445647.2017.1302364
dc.departamentoesGeologíaes_ES
dc.departamentoeuGeologiaes_ES


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© 2017 The Author(s). Published by Informa UK Limited, trading as Taylor & Francis Group on behalf of Journal of Maps
This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
Except where otherwise noted, this item's license is described as © 2017 The Author(s). Published by Informa UK Limited, trading as Taylor & Francis Group on behalf of Journal of Maps This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.