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dc.contributor.authorAndonaegui, P.
dc.date.accessioned2020-05-14T10:56:02Z
dc.date.available2020-05-14T10:56:02Z
dc.date.issued1991
dc.identifier.urihttp://hdl.handle.net/10272/17951
dc.description.abstractIn the plutonic complex of Mora-Gálvez (south Toledo) we have distinguished three types of granitoids: coarse grained granites, porphiritc granites and cordierite nodules leucogranites. Al/ of them are biotite-bearing and they usually have minor cordierite. Geochemically are peralouminous and their origin could be from melting of crustal rockses_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.otherGeochemistryes_ES
dc.subject.otherPeralouminous graniteses_ES
dc.subject.otherIberian Hercynian beltes_ES
dc.titleCaracterización geoquímica de los granitoides de Mora Gálvez (Toledo)es_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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Atribución-NoComercial-SinDerivadas 3.0 España
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