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dc.contributor.authorMuñoz, M.
dc.date.accessioned2020-07-09T09:01:07Z
dc.date.available2020-07-09T09:01:07Z
dc.date.issued1986
dc.identifier.urihttp://hdl.handle.net/10272/18491
dc.description.abstractThe basic intrusive bodies, from both Subbetic and Nevado-FiIábride domains, display analogous geological and petrographic features, as well as Ti, Zr, Y, Nb, trace elements contente All these aspects point to an alkaline intraplate magmatism, that can be related to a continental, tensional transcurrent zonees_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.otherMagnetism intraplatees_ES
dc.subject.otherTrace elementses_ES
dc.subject.otherBasic intrusionses_ES
dc.titleEstudio comparativo de los cuerpos intrusivos básicos asociados a los materiales de edad triásica de los dominios Subbético y Nevado-Filábride del sector Centro-Oriental de las cordilleras béticases_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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