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Magnetic structure of the Guitiriz and Hombreiro-Santa Eulalia de Pena granitic massifs (Lugo)

dc.contributor.authorAranguren, A.
dc.contributor.authorGarcía, C.
dc.contributor.authorTubía, José María
dc.date.accessioned2020-05-25T10:54:56Z
dc.date.available2020-05-25T10:54:56Z
dc.date.issued1991
dc.identifier.urihttp://hdl.handle.net/10272/18059
dc.description.abstractThe magnetic susceptibility anisotropy of 202 sites from the Variscan Guitiriz and HombreiroSanta Eulalia granites (Galicia, Spain) has been measured. The magnetic fabric is directly related to the field structures. The Guitiriz granite is characterized by Noth-South trending magnetic lineations whereas the Hombreiro-Santa Eulalia shows East-West trending magnetic lineationses_ES
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherGranitees_ES
dc.subject.otherMagnetic structurees_ES
dc.subject.otherGaliciaes_ES
dc.titleEstructura magnética de los macizos graníticos de Guitiriz y Hombreiro-Santa Eulalia de Pena (Lugo)es_ES
dc.titleMagnetic structure of the Guitiriz and Hombreiro-Santa Eulalia de Pena granitic massifs (Lugo)eng
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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